WEBVTT - How do we predict the weather?

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<v Speaker 1>When I moved to southern California, I felt this immediate,

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<v Speaker 1>immense relief, not just because I was free of the

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<v Speaker 1>tyranny of outside clothing, but because I was released from

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<v Speaker 1>the anxiety of not knowing if the weather was going

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<v Speaker 1>to ruin my plans. Were you planning an outdoor birthday

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<v Speaker 1>party for your toddler, No need to make backup plans

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<v Speaker 1>just in case it rains. Do you need to drive

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<v Speaker 1>a few hours away, No problem. You don't have to

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<v Speaker 1>worry that a snowstorm might make the roads impassable because

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<v Speaker 1>I could predict the weather myself since it was the

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<v Speaker 1>same every single day. But not all of us are

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<v Speaker 1>lucky enough to live in such calm climbs, so it's

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<v Speaker 1>still very important that we try to anticipate storms so

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<v Speaker 1>that they're less fortunate among us can be prepared. It's

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<v Speaker 1>not often described as important physics, but predicting the weather

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<v Speaker 1>is one of physics' great success stories. John Martin, professor

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<v Speaker 1>of atmospheric oceanic sciences, told me that weather predictions are

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<v Speaker 1>quote the most unheralded scientific advance of the second half

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<v Speaker 1>of the twentieth century. If you keep score every day,

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<v Speaker 1>I can't believe how well we predict the weather three

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<v Speaker 1>to five days in advance. In thirty years, we've gone

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<v Speaker 1>from predictions from one to two days to now five

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<v Speaker 1>to seven days. We have made unbelievable progress. So how

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<v Speaker 1>does that all work? What is the physics underlying the weather,

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<v Speaker 1>why has it gotten better? And what can we expect

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<v Speaker 1>into the future. I talked to Professor Martin and my

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<v Speaker 1>good friend Professor Jane Baldwin here at UC Irvine about

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<v Speaker 1>how the weather all works. So we'll dig into all

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<v Speaker 1>of that in today's episode, dedicated to all of y'all

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<v Speaker 1>who still experience regular weather. Welcome to Daniel and Kelly's

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<v Speaker 1>extraordinarily sunny universe.

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<v Speaker 2>Hello Kelly Leadersmith. I studied fites and space and I

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<v Speaker 2>love rainy days.

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<v Speaker 3>Hi.

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<v Speaker 1>I'm Daniel. I'm a particle physicist, and I can predict

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<v Speaker 1>the weather in California for the next one hundred years

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<v Speaker 1>with my eyes closed.

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<v Speaker 2>How boring, how massively dull.

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<v Speaker 1>How wonderfully, delightfully, predictably, reliably boring.

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<v Speaker 2>Oh, you know, one of my favorite weather moments, I

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<v Speaker 2>have to admit, was a southern California morning. So I

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<v Speaker 2>was a visiting scholar at the University of California, Santa

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<v Speaker 2>Barbara for a little while, and I had an office

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<v Speaker 2>that was like right out on the ocean. Was amazing.

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<v Speaker 2>And when I was driving in one day, there was

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<v Speaker 2>just a little bit of water on the ground and

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<v Speaker 2>the car tires were kicking up a little bit of

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<v Speaker 2>a spray, and there were literally rainbows following all of

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<v Speaker 2>the cars into school. And then I got out of

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<v Speaker 2>the car and the rain had stopped, and there was

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<v Speaker 2>a rainbow over the ocean and there were hummingbirds and

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<v Speaker 2>it was like a Disney movie scene. I expected like

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<v Speaker 2>a bunny to hop out and be like, can I

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<v Speaker 2>help you with anything? Anyway, it was. It was kind

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<v Speaker 2>of magical. I'll give you that.

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<v Speaker 1>California is heaven. Yes, what happens when you die in

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<v Speaker 1>Virginia is you end up in California.

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<v Speaker 2>Do you know that not all California as southern California.

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<v Speaker 1>I mean all of real California.

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<v Speaker 2>Oh, I see, because northern California's got some weather.

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<v Speaker 1>You're absolutely right. In fact, I heard Katrina say something

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<v Speaker 1>really insightful the other day. You know, she's from northern California.

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<v Speaker 1>But now we've lived in southern California for quite a while,

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<v Speaker 1>and she said to somebody that she's now a complete

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<v Speaker 1>Californian because she's lived in both northern and southern California.

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<v Speaker 1>And I was like, Oh, that's cool. She's like accepted

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<v Speaker 1>southern California, which is hard for Northern California's I'm aware, yes,

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<v Speaker 1>not everything is Southern California unfortunately.

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<v Speaker 2>Oh I really like the variability Virginia weather is amazing

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<v Speaker 2>for me. But so my question for you is, what

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<v Speaker 2>is the worst weather situation that you've experienced?

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<v Speaker 1>Great question. I was on the East coast, of course,

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<v Speaker 1>you're doing a college tour with my son, and we

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<v Speaker 1>were in Massachusetts. I think we were visiting Amherst or

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<v Speaker 1>maybe it was Williams, I don't remember. And there was

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<v Speaker 1>some freak tornado which tore up a bunch of trees

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<v Speaker 1>and knocked down a bunch of power lines and there

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<v Speaker 1>was no power in the whole town for like almost

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<v Speaker 1>half a day. It was crazy and the winds were

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<v Speaker 1>insane and it felt a little scary, like we saw

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<v Speaker 1>like huge branches flying by the window.

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<v Speaker 2>Yeah, yep.

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<v Speaker 1>And he didn't end up going to school there.

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<v Speaker 2>Yeah, I get that. I get that. So we lived

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<v Speaker 2>in Alabama, Tuscaloosa, and we moved there pretty soon after

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<v Speaker 2>that giant tornado that like made the news, and you

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<v Speaker 2>could see the path of the tornado because like, you know,

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<v Speaker 2>you'd be driving through an area with lots of like

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<v Speaker 2>you know, Starbucks, Panera, lots of stores or whatever, and

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<v Speaker 2>then suddenly there would be a like air an opening

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<v Speaker 2>in between all of the stores with nothing, and like

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<v Speaker 2>the tornado had just gone through there and just absolutely

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<v Speaker 2>picked up and thrown everything that was in there, and

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<v Speaker 2>even after they cleaned it out, there were still, you know,

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<v Speaker 2>you could tell where the tornado had gone. And we

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<v Speaker 2>were also in Houston during some pretty bad storms and

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<v Speaker 2>we had the kids and our dog and our cats

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<v Speaker 2>in a little hallway in the interior of the house

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<v Speaker 2>and my in laws were visiting, and my mother in

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<v Speaker 2>law was so sweet. She like looked around and she

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<v Speaker 2>she was trying to see, you know, who could get

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<v Speaker 2>hurt and how, And she gave her glasses to Zach

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<v Speaker 2>in case there was any like flying glass and she

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<v Speaker 2>just insisted that he have her glasses. And I was

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<v Speaker 2>like in that moment, I was like, gosh, you are

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<v Speaker 2>the sweetest person in the whole world, Like you are

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<v Speaker 2>thinking about the tiny little things you could do to

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<v Speaker 2>help the people around you, and anyway, she's she's the best.

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<v Speaker 1>Yeah, but we've all been caught in surprise weather, right.

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<v Speaker 1>I remember going backpacking in Arkansas one time and being

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<v Speaker 1>caught in a snowstorm and the temperatures dropped into the

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<v Speaker 1>teens and we weren't one hundred percent sure we were

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<v Speaker 1>going to make it. Oh, and everybody's been, like, you know,

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<v Speaker 1>caught in a snowstorm or a rainstorm or in a

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<v Speaker 1>heat wave. Right, And these things are exciting, they can

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<v Speaker 1>be dramatic, but they can also be very dangerous, right.

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<v Speaker 2>Yeah.

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<v Speaker 1>People die in these crazy weather storms, and so it's

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<v Speaker 1>valuable to be able to know in advance what's going

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<v Speaker 1>to happen, not just so you can plain your picnics,

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<v Speaker 1>but also you can survive the increasingly dramatic weather that

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<v Speaker 1>we're all facing as the planet warms.

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<v Speaker 2>Yeah, that's right, more severe weather is becoming more common.

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<v Speaker 2>And so today we're going to talk about how good

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<v Speaker 2>we are at making predictions and how we go about

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<v Speaker 2>making those predictions exactly.

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<v Speaker 1>And I wanted to pull back the curtain on like

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<v Speaker 1>the science of this, how does this actually happen, What

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<v Speaker 1>are we doing, why is it hard? What are the challenges?

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<v Speaker 1>What improvements might we be seeing in the next five

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<v Speaker 1>or ten years. What problems are just fundamentally impossible and

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<v Speaker 1>might never be solved. And so today we're going to

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<v Speaker 1>dig into science of all that. But before we explain

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<v Speaker 1>to you how the experts do it, I was wondering

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<v Speaker 1>what everybody knew about how weather predictions happen. How do

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<v Speaker 1>those numbers end up on your phone? So I went

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<v Speaker 1>out there to ask our listeners what they knew about

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<v Speaker 1>how we predict the weather. If you would like to

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<v Speaker 1>answer these kind of questions for a future episode, don't

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<v Speaker 1>be shy, right to us two questions at Danielankelly dot org.

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<v Speaker 1>We will send you fun questions every week in your inbox.

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<v Speaker 1>In the meantime, think about it for a minute. What

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<v Speaker 1>do you know about how we predict the weather? Here's

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<v Speaker 1>what our listeners had to say. Sophisticated computer models, which

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<v Speaker 1>with an understanding if case theory, allows us to understand

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<v Speaker 1>the limitations.

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<v Speaker 4>Predicting the weather is like quantum particles.

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<v Speaker 1>There are many probabilities, but it is not known until

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<v Speaker 1>it is observed. Meteorologists they look at the current weather,

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<v Speaker 1>and they try to predict it by looking at the

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<v Speaker 1>moving clouds and all of.

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<v Speaker 3>That, by measuring with velocity and atmospheric pressure and maybe

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<v Speaker 3>modeling these that in supercomputers.

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<v Speaker 1>When a cow lies down in the field, it's going

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<v Speaker 1>to and when my knee aches, it's gonna snow.

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<v Speaker 4>Running multiple models.

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<v Speaker 3>Big computers, really really big computers.

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<v Speaker 4>Feed dad data, two complicated models that run on very

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<v Speaker 4>parfa spoken.

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<v Speaker 1>Pere i'd say, with surface measurements, satellite information and sophisticated

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<v Speaker 1>models and perhaps even artificial.

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<v Speaker 4>Intelligence observations taken by ships, planes, ground stations, satellites combined

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<v Speaker 4>with models built by really really smart people that run

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<v Speaker 4>on some of the fastest computers that humans have ever built.

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<v Speaker 1>There are sophisticated bottles that use a wide range of

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<v Speaker 1>observational and predictive inputs.

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<v Speaker 4>By observing weather patterns and the types of whether those

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<v Speaker 4>patterns tend to bring.

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<v Speaker 2>So I don't know if there's actually like scientific evidence

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<v Speaker 2>that sometimes knees will ache if like a stormfront is

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<v Speaker 2>coming through. But I have to admit that there's a

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<v Speaker 2>part of me that really hopes that if I get

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<v Speaker 2>arthright is when I'm older, I do have the ability

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<v Speaker 2>to tell when the weather's come in because I'll feel

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<v Speaker 2>like I'm really intimately connected to my environment. Oh, the

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<v Speaker 2>knees acted up again. Storms come and get the goats

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<v Speaker 2>in the barn.

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<v Speaker 1>I think that really shows your fundamental optimistic nature, Kelly,

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<v Speaker 1>because you're like, oh, I forget arthritis. There'll be a

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<v Speaker 1>silver lining. I can predict the weather.

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<v Speaker 2>You know, life is easier when you try to see

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<v Speaker 2>the silver lining.

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<v Speaker 1>That's wonderful.

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<v Speaker 2>But our audience had great answers, and they were, you know,

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<v Speaker 2>a lot of them said, you know exactly the right thing,

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<v Speaker 2>which is you've got to have data. Those are the

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<v Speaker 2>observations and you feed them into computers.

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<v Speaker 1>Yeah, essentially, and that's the big picture, not just of

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<v Speaker 1>weather prediction but any kind of prediction. There are two

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<v Speaker 1>fundamental ingredients to how you make a prediction. There's the

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<v Speaker 1>models and then there's the data. So let's take those

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<v Speaker 1>each in turn. When we say the models, we mean

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<v Speaker 1>like we're running a computer simulation or you're calculating things

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<v Speaker 1>on paper. Fundamentally, this is encoding the rules of the

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<v Speaker 1>system what the future can be given what the past was.

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<v Speaker 1>And this doesn't have to be some really complicated thing

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<v Speaker 1>like the weather over ist endbull. Think about a much

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<v Speaker 1>simpler situation, like you're tossing a ball in your backyard.

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<v Speaker 1>You want to know where does it go? Well, the

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<v Speaker 1>laws of physics predict the future, right, this is the model.

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<v Speaker 1>These are the rules that tell you how the past

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<v Speaker 1>becomes the future. Right. And in this case it's simple.

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<v Speaker 1>It's a parabola. It flies through the air. Things to

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<v Speaker 1>keep in mind here, though, is that a model like

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<v Speaker 1>this is always approximate. If I use f eicals MA

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<v Speaker 1>and I just account for gravity, ignore air resistance. When

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<v Speaker 1>I'm describing the ball, I'm going to get a quick answer,

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<v Speaker 1>and it's gonna be pretty good. It's not going to

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<v Speaker 1>be exactly bang on correct. It can't account for everything,

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<v Speaker 1>all the little wind gusts and the air resistance and

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<v Speaker 1>the slight change in humidity and maybe the spin on

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<v Speaker 1>the ball. My model ignores some details, and that's crucial. Right.

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<v Speaker 1>If I included every single particle in the backyard, I

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<v Speaker 1>would never get a calculation. So in order to make

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<v Speaker 1>this tractable, I got to simplify the problem. I got

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<v Speaker 1>to pull out the things that are important and ignore

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<v Speaker 1>the things I think are unimportant. Because I don't think

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<v Speaker 1>they're going to make a big enough difference in the answer.

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<v Speaker 1>And this is where the juice is. This is what

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<v Speaker 1>physics is, right. Physics is taking the universe and simplifying

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<v Speaker 1>it into a model that represents the bits you're excited about,

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<v Speaker 1>the bits you think are interesting and irrelevant, and then

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<v Speaker 1>you use those rules and manipulate it. That's your model

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<v Speaker 1>of the universe, and the model gives you an answer,

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<v Speaker 1>and hopefully, if the model is close enough to your

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<v Speaker 1>description of the universe, the answer you get from the

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<v Speaker 1>model is similar to the answer in the actual universe.

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<v Speaker 2>So one thing I think that's amazing is that something

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<v Speaker 2>as simple as throwing a ball up in the air

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<v Speaker 2>and then seeing where it lands is something we can't

0:11:37.840 --> 0:11:40.600
<v Speaker 2>completely model because there's so many complicating things. And now

0:11:40.640 --> 0:11:44.119
<v Speaker 2>you're talking about weather, which is so much more complicated

0:11:44.120 --> 0:11:46.480
<v Speaker 2>and requires so many more inputs. And of course you

0:11:46.520 --> 0:11:48.760
<v Speaker 2>can update your model. So you know, if you threw

0:11:48.800 --> 0:11:50.160
<v Speaker 2>the ball in the air and you were like, you

0:11:50.160 --> 0:11:52.679
<v Speaker 2>know what, it's a windy day, I absolutely need to

0:11:52.679 --> 0:11:55.920
<v Speaker 2>add wind. Now you've learned something, you add wind, and

0:11:55.960 --> 0:11:58.160
<v Speaker 2>so you know, it's an iterative process where you keep

0:11:58.200 --> 0:12:01.040
<v Speaker 2>trying to say what is in important and do I

0:12:01.120 --> 0:12:03.480
<v Speaker 2>need to include it? And does it make my predictions better?

0:12:03.640 --> 0:12:07.360
<v Speaker 2>But I also will note that you put predicting weather

0:12:08.000 --> 0:12:11.800
<v Speaker 2>under the physics umbrella. You think you guys get to

0:12:11.800 --> 0:12:13.000
<v Speaker 2>claim weather predictions.

0:12:13.600 --> 0:12:15.880
<v Speaker 1>I mean, we're not using economics to predict the weather.

0:12:16.520 --> 0:12:19.280
<v Speaker 1>What else is in the running for taking credit for

0:12:19.320 --> 0:12:21.880
<v Speaker 1>predicting the weather? Is it chemistry?

0:12:22.320 --> 0:12:24.880
<v Speaker 2>I feel like that also is some ecology, you know,

0:12:25.080 --> 0:12:26.760
<v Speaker 2>like because you're tracking.

0:12:26.520 --> 0:12:27.960
<v Speaker 1>Like cowfarts or something.

0:12:28.200 --> 0:12:29.679
<v Speaker 2>No, no, you like, you know, a.

0:12:29.679 --> 0:12:33.080
<v Speaker 1>Fart player role. Actually, so do you think.

0:12:33.000 --> 0:12:36.720
<v Speaker 2>That Noah has cow farts in their weather prediction models?

0:12:38.200 --> 0:12:42.319
<v Speaker 1>I think the climate models do include bovine methane emissions. Yes,

0:12:42.640 --> 0:12:45.880
<v Speaker 1>so not the daily predictions, but the bigger trends. Yes,

0:12:45.960 --> 0:12:48.760
<v Speaker 1>cow farts do help determine the future of our planet.

0:12:48.960 --> 0:12:49.360
<v Speaker 2>Amazing.

0:12:49.360 --> 0:12:50.920
<v Speaker 1>I want to go back to the point you made earlier.

0:12:51.000 --> 0:12:54.360
<v Speaker 1>You're exactly right that we're always approximating, and not just

0:12:54.440 --> 0:12:58.199
<v Speaker 1>when we're doing the weather, not just when we're tossing balls, always,

0:12:58.720 --> 0:13:03.160
<v Speaker 1>every single time, every model is approximation. There's this famous phrase.

0:13:03.160 --> 0:13:05.480
<v Speaker 1>I a memember who said it, like all models are wrong,

0:13:05.640 --> 0:13:08.360
<v Speaker 1>some of them are useful, even our description of like

0:13:08.559 --> 0:13:11.240
<v Speaker 1>the fundamental particles in the universe. As far as we know,

0:13:11.480 --> 0:13:15.920
<v Speaker 1>these are approximations. Every bit of science we have has

0:13:16.040 --> 0:13:19.720
<v Speaker 1>boundaries of where it's relevant because there are approximations made

0:13:20.080 --> 0:13:23.920
<v Speaker 1>when we construct those models everything, literally everything. We have

0:13:24.000 --> 0:13:27.680
<v Speaker 1>no piece of science that isn't an approximation of the universe.

0:13:28.280 --> 0:13:31.120
<v Speaker 1>Maybe one day we have a theory of everything, and

0:13:31.160 --> 0:13:34.600
<v Speaker 1>it's beautiful and we can do exact calculations on very

0:13:34.720 --> 0:13:38.440
<v Speaker 1>very simple situations. But we're not there. We may never

0:13:38.520 --> 0:13:40.920
<v Speaker 1>be there, and even if we are there, it will

0:13:40.960 --> 0:13:43.920
<v Speaker 1>be totally impractical for anything useful. Like you couldn't use

0:13:44.400 --> 0:13:47.360
<v Speaker 1>string theory to predict the path of a hurricane because

0:13:47.640 --> 0:13:51.040
<v Speaker 1>the complexity would be insane, Right, how many strings are

0:13:51.040 --> 0:13:53.640
<v Speaker 1>you modeling? The amount of computation required to do it

0:13:53.720 --> 0:13:57.480
<v Speaker 1>exactly would be impossible. So it's always an approximation. It's

0:13:57.520 --> 0:14:00.920
<v Speaker 1>just a question of which approximations. That's where the science

0:14:00.960 --> 0:14:03.240
<v Speaker 1>comes in, like which ones are important. Having a nose

0:14:03.840 --> 0:14:06.720
<v Speaker 1>for what to approximate and what not to approximate, that's

0:14:06.720 --> 0:14:09.320
<v Speaker 1>what helps some scientists make more progress than others.

0:14:09.480 --> 0:14:11.440
<v Speaker 2>Yeah, And I think another thing to just sort of

0:14:11.480 --> 0:14:14.800
<v Speaker 2>note is that because this is a human endeavor. Sometimes

0:14:14.920 --> 0:14:17.959
<v Speaker 2>you're limited by what you can afford to get data

0:14:18.000 --> 0:14:20.200
<v Speaker 2>on you know, like maybe you do want to know

0:14:20.640 --> 0:14:23.360
<v Speaker 2>how much cows are farting, but in order to get

0:14:23.360 --> 0:14:26.440
<v Speaker 2>that data, you would need seventy billion dollars so that

0:14:27.040 --> 0:14:30.320
<v Speaker 2>farmers could attach sensors to the rear end of every cow.

0:14:30.400 --> 0:14:33.400
<v Speaker 2>And so, like, you know, sometimes you know there's data

0:14:33.440 --> 0:14:34.920
<v Speaker 2>you want, but you can't get it because there's not

0:14:35.040 --> 0:14:37.080
<v Speaker 2>enough money or it's not possible. Maybe one day you

0:14:37.080 --> 0:14:39.000
<v Speaker 2>can get it, Maybe those sensors will become cheap.

0:14:39.160 --> 0:14:42.080
<v Speaker 1>Is seventy billion dollars your like a fantastical number for

0:14:42.120 --> 0:14:44.360
<v Speaker 1>some like absurd amount of money for a science experiment?

0:14:44.920 --> 0:14:47.640
<v Speaker 2>Yeah, I guess that's wow. Yeah what is yours? I

0:14:47.640 --> 0:14:49.280
<v Speaker 2>guess you're a physicist, so it's going to be like.

0:14:49.360 --> 0:14:52.680
<v Speaker 1>Well, that's embarrassing because our next project is one hundred

0:14:52.720 --> 0:14:56.600
<v Speaker 1>billion dollars, So we're like already above the Kelly threshold

0:14:56.640 --> 0:14:58.440
<v Speaker 1>for like absurd amounts of money.

0:14:58.600 --> 0:15:01.400
<v Speaker 2>But wait, like, okay, but that's not like your personal project.

0:15:01.440 --> 0:15:04.560
<v Speaker 2>That's like LHC or like a new particle collider or something.

0:15:04.640 --> 0:15:07.240
<v Speaker 1>Right, Yeah, the new next particle collider budget is about

0:15:07.280 --> 0:15:10.440
<v Speaker 1>one hundred billion, Yes exactly, so more than a planet

0:15:10.480 --> 0:15:12.200
<v Speaker 1>wide cow farts sensor network.

0:15:12.360 --> 0:15:15.280
<v Speaker 2>Well, you guys better make some really important discoveries with

0:15:15.320 --> 0:15:17.880
<v Speaker 2>that money. Otherwise I'm disappointed because I want to know

0:15:17.920 --> 0:15:19.120
<v Speaker 2>what's happening with the cow farts.

0:15:20.280 --> 0:15:22.400
<v Speaker 1>But you bring up another point, which is the data.

0:15:22.560 --> 0:15:25.160
<v Speaker 1>So models are useful. There are a system that tell

0:15:25.240 --> 0:15:28.640
<v Speaker 1>us how the past becomes the future, but you also

0:15:28.680 --> 0:15:31.640
<v Speaker 1>need some data so you know which past you had. Right,

0:15:32.080 --> 0:15:36.680
<v Speaker 1>models describe essentially any possible universe. The rules determine which

0:15:36.840 --> 0:15:39.760
<v Speaker 1>set of universes we might live in, but the data

0:15:39.800 --> 0:15:42.760
<v Speaker 1>constrain it. It tells us which past we had. So

0:15:42.800 --> 0:15:45.080
<v Speaker 1>the rules tell you how the past becomes the future,

0:15:45.280 --> 0:15:47.680
<v Speaker 1>but you need to know which past we were in

0:15:47.720 --> 0:15:50.640
<v Speaker 1>so we know which future will have. So in our

0:15:50.680 --> 0:15:53.320
<v Speaker 1>ball tossing analogy, there's lots of different ways that could

0:15:53.320 --> 0:15:55.440
<v Speaker 1>toss a ball. I Coatalla said high or low, or

0:15:55.440 --> 0:15:58.520
<v Speaker 1>fast or slow or east or west. The rules connect

0:15:58.600 --> 0:16:02.360
<v Speaker 1>the initial conditions that data the past to the future.

0:16:02.560 --> 0:16:05.040
<v Speaker 1>But you need to know where did I throw the ball.

0:16:05.160 --> 0:16:07.720
<v Speaker 1>So if I'm writing a simulation of that ball toss,

0:16:07.800 --> 0:16:09.360
<v Speaker 1>I got to encode in the laws of physics. But

0:16:09.400 --> 0:16:11.320
<v Speaker 1>then I need a data point. I need to say

0:16:11.480 --> 0:16:13.560
<v Speaker 1>the ball was here and it was moving in this

0:16:13.640 --> 0:16:16.920
<v Speaker 1>direction at this velocity. Then I can predict the future.

0:16:17.280 --> 0:16:21.160
<v Speaker 1>Without that, it's useless. Right, So you need these two components.

0:16:21.160 --> 0:16:24.000
<v Speaker 1>You need the models, plus you need the data, and

0:16:24.040 --> 0:16:27.520
<v Speaker 1>then you need more data. Say I'm predicting the ball toss,

0:16:27.680 --> 0:16:29.560
<v Speaker 1>I want to check in halfway and say, hey, it's

0:16:29.600 --> 0:16:32.960
<v Speaker 1>my model correct, doesn't need an adjustment. A way to

0:16:33.000 --> 0:16:35.920
<v Speaker 1>improve your modeling is to shorten the prediction time, to

0:16:35.920 --> 0:16:38.000
<v Speaker 1>say I'm not going to predict the whole path. I'm

0:16:38.000 --> 0:16:39.440
<v Speaker 1>going to predict the second and then I'm going to

0:16:39.480 --> 0:16:41.400
<v Speaker 1>take a measurement and if it's off, I'm going to

0:16:41.440 --> 0:16:43.920
<v Speaker 1>correct it so that if my model has veered off

0:16:43.920 --> 0:16:47.600
<v Speaker 1>from reality, it doesn't get further off. And so the

0:16:47.600 --> 0:16:49.640
<v Speaker 1>more data you have, the better your model is going

0:16:49.680 --> 0:16:52.280
<v Speaker 1>to be. So you need these two elements dancing together,

0:16:52.560 --> 0:16:54.000
<v Speaker 1>the models and the data.

0:16:54.160 --> 0:16:56.600
<v Speaker 2>Yeah, and I checked my weather app today and the

0:16:56.640 --> 0:16:59.600
<v Speaker 2>prediction for tomorrow was changed, And so I'm guessing we

0:16:59.640 --> 0:17:03.280
<v Speaker 2>do this same thing with weather Way update. So I

0:17:03.280 --> 0:17:05.200
<v Speaker 2>think we should talk in a second about what kinds

0:17:05.200 --> 0:17:08.720
<v Speaker 2>of data we collect to help us inform models. But

0:17:08.840 --> 0:17:11.080
<v Speaker 2>I guess my first question is we've talked about models

0:17:11.119 --> 0:17:13.879
<v Speaker 2>in general. How long have we been trying to model weather?

0:17:14.760 --> 0:17:15.840
<v Speaker 2>Aristotle problems, So.

0:17:18.400 --> 0:17:20.800
<v Speaker 1>People have had some crazy ideas about the weather for

0:17:20.880 --> 0:17:24.560
<v Speaker 1>thousands of years. The first real weather models were conceived

0:17:24.600 --> 0:17:28.159
<v Speaker 1>of in the nineteen twenties. And remember we didn't have

0:17:28.200 --> 0:17:31.080
<v Speaker 1>computers really until the fifties or so, so this was

0:17:31.119 --> 0:17:34.480
<v Speaker 1>like a conception and somebody did a proof of principal prediction.

0:17:34.800 --> 0:17:37.760
<v Speaker 1>They tried to predict the weather six hours later. They

0:17:37.800 --> 0:17:39.920
<v Speaker 1>took a bunch of measurements and said, let's try to

0:17:39.960 --> 0:17:43.320
<v Speaker 1>do some calculations. We have an early model. That calculation

0:17:43.480 --> 0:17:44.760
<v Speaker 1>took six weeks.

0:17:45.200 --> 0:17:46.240
<v Speaker 2>So not helpful.

0:17:46.600 --> 0:17:50.000
<v Speaker 1>Not helpful exactly, but they did it and it wasn't terrible,

0:17:50.080 --> 0:17:51.919
<v Speaker 1>and they sort of proved like, hey, you know, if

0:17:51.960 --> 0:17:54.679
<v Speaker 1>you could do this calculation more quickly, then maybe you

0:17:54.680 --> 0:17:57.479
<v Speaker 1>could even know the weather in advance. Oh my gosh,

0:17:57.600 --> 0:18:00.840
<v Speaker 1>what an idea. Right, Yeah, it was until the nineteen

0:18:00.920 --> 0:18:03.399
<v Speaker 1>fifties that we had the first computing models to do

0:18:03.440 --> 0:18:07.359
<v Speaker 1>these calculations. So we can make predictions in time shorter

0:18:07.440 --> 0:18:10.080
<v Speaker 1>than the prediction period. You could have enough data and

0:18:10.200 --> 0:18:13.120
<v Speaker 1>run your model and get an answer before the universe

0:18:13.200 --> 0:18:16.520
<v Speaker 1>revealed it, right, that's that's a prediction instead of a

0:18:16.560 --> 0:18:17.280
<v Speaker 1>post addiction.

0:18:18.320 --> 0:18:18.800
<v Speaker 2>That's better.

0:18:18.840 --> 0:18:21.439
<v Speaker 1>So we've been doing this for decades and the last

0:18:21.560 --> 0:18:24.119
<v Speaker 1>you know, seventy years or so have been improving the

0:18:24.160 --> 0:18:26.160
<v Speaker 1>models and improving the data.

0:18:26.200 --> 0:18:28.680
<v Speaker 2>Man, it's exciting to think that we, you know, we're

0:18:28.720 --> 0:18:33.280
<v Speaker 2>going from slide rules to make these predictions to massive supercomputers.

0:18:33.880 --> 0:18:36.680
<v Speaker 2>I'm appreciating my weather apps a bit more.

0:18:37.960 --> 0:18:40.679
<v Speaker 1>And also, like, six weeks sounds ridiculous. I don't know

0:18:40.680 --> 0:18:42.320
<v Speaker 1>that I could do that in six weeks. Oh, it's

0:18:42.320 --> 0:18:45.800
<v Speaker 1>an amazing calculation. And think about like not just the ideas,

0:18:45.800 --> 0:18:49.040
<v Speaker 1>but all the grunt work doing those calculations and the

0:18:49.119 --> 0:18:51.679
<v Speaker 1>human error that's possible. Like, it's amazing they did it

0:18:51.680 --> 0:18:54.399
<v Speaker 1>in six weeks, you know, So don't laugh at that.

0:18:54.600 --> 0:18:57.840
<v Speaker 2>Absolutely, So we've been doing this since the nineteen fifties.

0:18:57.920 --> 0:19:00.439
<v Speaker 2>Let's talk about what kind of data we're collect to

0:19:00.520 --> 0:19:02.960
<v Speaker 2>inform these models when we get back from the break.

0:19:22.760 --> 0:19:24.840
<v Speaker 2>All right, and we are back, So now we're going

0:19:24.880 --> 0:19:27.280
<v Speaker 2>to talk about the kinds of data that we use

0:19:27.400 --> 0:19:31.200
<v Speaker 2>to make weather predictions. And I'm gonna bet it involves satellites.

0:19:33.160 --> 0:19:36.640
<v Speaker 1>Always going with space first, right, yep, yep. It does

0:19:36.680 --> 0:19:41.359
<v Speaker 1>involve satellites, but there's an amazing, incredible variety of data

0:19:41.400 --> 0:19:44.160
<v Speaker 1>sources we have to understand the weather. And yet still

0:19:44.160 --> 0:19:47.520
<v Speaker 1>it's not nearly enough. Right as you'll hear, our weather

0:19:47.560 --> 0:19:50.399
<v Speaker 1>prediction would be so much better if we had more data.

0:19:50.480 --> 0:19:53.280
<v Speaker 1>We're really limited by the data. But we have lots

0:19:53.280 --> 0:19:56.040
<v Speaker 1>of different kinds. We have weather stations on the surface

0:19:56.160 --> 0:19:58.520
<v Speaker 1>and so a lot of these are called like automatic

0:19:58.520 --> 0:20:01.560
<v Speaker 1>weather stations that are scattered across the country. They're just

0:20:01.560 --> 0:20:04.800
<v Speaker 1>basically a bunch of sensors with a battery and like

0:20:04.880 --> 0:20:08.040
<v Speaker 1>either a wind turbine or a solar panel to get power,

0:20:08.520 --> 0:20:11.960
<v Speaker 1>and they measure things like temperature and pressure and wind

0:20:12.040 --> 0:20:16.359
<v Speaker 1>speed and precipitation, just the raw measurements you need to know,

0:20:16.400 --> 0:20:19.320
<v Speaker 1>like what's going on out there, what is the state

0:20:19.520 --> 0:20:22.480
<v Speaker 1>of the weather right now, because again, if you want

0:20:22.520 --> 0:20:24.560
<v Speaker 1>to predict the future weather, you've got to know what's

0:20:24.560 --> 0:20:25.919
<v Speaker 1>going on right now.

0:20:26.119 --> 0:20:28.359
<v Speaker 2>So is this like a citizen science thing where like

0:20:28.480 --> 0:20:31.040
<v Speaker 2>I could purchase one of these weather stations and hook

0:20:31.080 --> 0:20:33.400
<v Speaker 2>it into what's happening at like the national level.

0:20:33.600 --> 0:20:35.879
<v Speaker 1>Yes and no. So there are a few sort of

0:20:35.880 --> 0:20:39.200
<v Speaker 1>official stations. There's a bunch of different networks. The highest

0:20:39.280 --> 0:20:42.760
<v Speaker 1>quality ones. There's like ten thousand of these scattered around

0:20:42.760 --> 0:20:45.880
<v Speaker 1>the earth, and they're operated by weather services and government agencies.

0:20:46.520 --> 0:20:49.320
<v Speaker 1>But there's a bigger network of like quarter million of

0:20:49.359 --> 0:20:52.080
<v Speaker 1>these things. Some of these are personal weather stations that yeah,

0:20:52.240 --> 0:20:55.760
<v Speaker 1>people just build and publish the data. And there's an

0:20:55.800 --> 0:21:02.200
<v Speaker 1>amazing network it's called COCO ras COOCOHS Community Collaborative Rain,

0:21:02.400 --> 0:21:05.480
<v Speaker 1>Hail and snow Wow. If you can just like build

0:21:05.520 --> 0:21:09.000
<v Speaker 1>your own device and add it to the network and contribute,

0:21:09.040 --> 0:21:12.160
<v Speaker 1>and I think that's super awesome because it's definitely limited

0:21:12.480 --> 0:21:16.200
<v Speaker 1>by the data we have. One problem is that these

0:21:16.240 --> 0:21:18.200
<v Speaker 1>things tend to be where the people are, Like we

0:21:18.280 --> 0:21:20.960
<v Speaker 1>have a few, you know, top of Mount Washington or whatever,

0:21:21.240 --> 0:21:23.400
<v Speaker 1>but mostly these things are put up by people where

0:21:23.400 --> 0:21:26.840
<v Speaker 1>people are near, and so like there's lots in India,

0:21:26.920 --> 0:21:30.879
<v Speaker 1>for example, but very few across Siberia, And often the

0:21:30.880 --> 0:21:33.879
<v Speaker 1>best ones are at places like airports. Airports really need

0:21:33.920 --> 0:21:36.679
<v Speaker 1>to know whether so they have excellent weather stations. But

0:21:36.840 --> 0:21:39.760
<v Speaker 1>like the weather at LaGuardia is not the same as

0:21:39.760 --> 0:21:43.440
<v Speaker 1>the weather in Manhattan, and so often the airport weather

0:21:43.480 --> 0:21:46.400
<v Speaker 1>stations are very very precise and used heavily in the models,

0:21:46.840 --> 0:21:48.760
<v Speaker 1>but they're not giving you the measurements exactly where you

0:21:48.800 --> 0:21:49.399
<v Speaker 1>want them to be.

0:21:49.640 --> 0:21:53.240
<v Speaker 2>Okay, So is that a problem for just the people

0:21:53.240 --> 0:21:56.840
<v Speaker 2>who are in areas where there's not enough weather detectors

0:21:57.359 --> 0:21:59.480
<v Speaker 2>or is that a problem for all of us, because

0:21:59.520 --> 0:22:03.119
<v Speaker 2>what's happened in Siberia is important to what's happening in India.

0:22:03.240 --> 0:22:06.520
<v Speaker 1>Yeah, what happens in Siberia doesn't stay in Siberia. Unfortunately.

0:22:08.960 --> 0:22:12.840
<v Speaker 1>It contributes to uncertainty and error across the model. And

0:22:12.880 --> 0:22:14.600
<v Speaker 1>the Earth is one big system, which is why you

0:22:14.600 --> 0:22:16.359
<v Speaker 1>can't just be like, I'm only going to predict the

0:22:16.400 --> 0:22:18.800
<v Speaker 1>weather Manhattan. I only need to think about Manhattan. You

0:22:18.880 --> 0:22:20.800
<v Speaker 1>need to model the whole planet in order to get

0:22:20.800 --> 0:22:23.720
<v Speaker 1>the weather in Manhattan. So yeah, absolutely, And that's why

0:22:23.760 --> 0:22:25.960
<v Speaker 1>we have lots of different kinds of sensors, not just

0:22:26.040 --> 0:22:30.080
<v Speaker 1>these automatic weather stations. We also have things like weather radar,

0:22:30.160 --> 0:22:32.359
<v Speaker 1>and you might have seen these on your local weather channel.

0:22:32.400 --> 0:22:35.399
<v Speaker 1>Like let's look at the Doppler, this measure of precipitation.

0:22:35.520 --> 0:22:39.760
<v Speaker 1>It also measures the velocity of those rain drops. And

0:22:39.800 --> 0:22:41.600
<v Speaker 1>this is a really cool story because it comes out

0:22:41.600 --> 0:22:44.399
<v Speaker 1>of World War Two. It's another example of like reusing

0:22:44.480 --> 0:22:47.719
<v Speaker 1>military technology and infrastructure after World War two to do

0:22:47.800 --> 0:22:48.400
<v Speaker 1>some science.

0:22:48.600 --> 0:22:54.440
<v Speaker 2>Thank you war Oh boy, hot take pull it back.

0:22:55.119 --> 0:22:58.480
<v Speaker 1>Well, there you are again finding the silver lining. Tens

0:22:58.480 --> 0:23:02.040
<v Speaker 1>of millions of people died, but we have better weather predictions.

0:23:02.520 --> 0:23:05.280
<v Speaker 1>So the way radar works is that it sends these

0:23:05.600 --> 0:23:09.159
<v Speaker 1>pulses of microwave radiation. The wavelengths are like one to

0:23:09.200 --> 0:23:12.239
<v Speaker 1>ten centimeters, that's the microwave region. And it sends a

0:23:12.240 --> 0:23:14.679
<v Speaker 1>pulse for like a microsecond, and then it listens for

0:23:14.760 --> 0:23:18.680
<v Speaker 1>return signals. So like it sends this pulse and rain

0:23:18.800 --> 0:23:22.280
<v Speaker 1>drops will reflect, so it gets the signal back and

0:23:22.320 --> 0:23:24.439
<v Speaker 1>it listens for like a few milliseconds, and then it

0:23:24.440 --> 0:23:27.439
<v Speaker 1>sends another pulse, and so it can tell where the

0:23:27.440 --> 0:23:30.520
<v Speaker 1>clouds are, and it can tell the velocity of those

0:23:30.520 --> 0:23:34.560
<v Speaker 1>clouds by the change in frequency. This is the Doppler effect, right,

0:23:34.560 --> 0:23:36.920
<v Speaker 1>And this is exactly the same effect as like stars

0:23:36.960 --> 0:23:39.200
<v Speaker 1>are moving away from you, so their light is red

0:23:39.240 --> 0:23:42.440
<v Speaker 1>shifted when the radar pulse comes back. If the frequency

0:23:42.480 --> 0:23:46.200
<v Speaker 1>is shifted, you can tell which direction that rain drop

0:23:46.359 --> 0:23:46.879
<v Speaker 1>is moving.

0:23:47.080 --> 0:23:50.119
<v Speaker 2>So that sounds complicated because like there's not just one

0:23:50.520 --> 0:23:52.720
<v Speaker 2>rain drop out there, there's a bunch and so I

0:23:52.720 --> 0:23:56.440
<v Speaker 2>can imagine like your pulse getting lost as it bounces

0:23:56.480 --> 0:23:58.920
<v Speaker 2>off of multiple rain drops and doesn't make it back

0:23:58.920 --> 0:24:01.000
<v Speaker 2>to you. What am I miss saying? This sounds hard?

0:24:01.119 --> 0:24:03.879
<v Speaker 1>No, it is hard, But you're not detecting individual rain drops.

0:24:03.880 --> 0:24:07.159
<v Speaker 1>You're detecting clouds mostly like which direction is this cloud going?

0:24:07.760 --> 0:24:10.399
<v Speaker 1>And you know, initially this was a problem because in

0:24:10.440 --> 0:24:12.680
<v Speaker 1>World War Two, radar operators were trying to use radar

0:24:12.720 --> 0:24:15.760
<v Speaker 1>to discover like enemy planes, and they noticed, like man,

0:24:15.880 --> 0:24:18.600
<v Speaker 1>clouds are getting in the way. And then other folks

0:24:18.680 --> 0:24:21.280
<v Speaker 1>were like, oh wait, you can use radar to see clouds. Awesome,

0:24:21.600 --> 0:24:25.960
<v Speaker 1>and so and so. Then after World War Two they

0:24:26.000 --> 0:24:28.359
<v Speaker 1>started using this to measure the velocity of clouds and

0:24:28.400 --> 0:24:31.360
<v Speaker 1>to see them. And there's this moment in like nineteen

0:24:31.480 --> 0:24:34.800
<v Speaker 1>sixty one when Hurricane Carlo was approaching the coast of

0:24:34.800 --> 0:24:37.320
<v Speaker 1>Texas and Dan Rather went down there to a weather

0:24:37.359 --> 0:24:40.400
<v Speaker 1>station and they were using radar to see the clouds

0:24:40.440 --> 0:24:42.480
<v Speaker 1>and to see their direction, and he had them drawn

0:24:42.520 --> 0:24:45.320
<v Speaker 1>like the coast of Texas over this image of the

0:24:45.400 --> 0:24:48.280
<v Speaker 1>hurricane that showed everybody like, wow, this is a massive

0:24:48.359 --> 0:24:51.840
<v Speaker 1>hurricane moving fast towards the shore and probably save thousands

0:24:51.880 --> 0:24:56.240
<v Speaker 1>of lives because he publicized this like incoming storm much

0:24:56.280 --> 0:24:59.040
<v Speaker 1>more rapidly than we could otherwise without this kind of technology.

0:24:59.320 --> 0:24:59.439
<v Speaker 3>Wo.

0:25:00.240 --> 0:25:01.920
<v Speaker 1>Yeah, this weather radar is really helpful.

0:25:02.040 --> 0:25:03.840
<v Speaker 2>Do you think it still has the same effector or

0:25:03.840 --> 0:25:05.639
<v Speaker 2>do you think people are just kind of like, oh,

0:25:05.680 --> 0:25:08.600
<v Speaker 2>there's hurricanes, I've seen them before. They get big, and

0:25:08.640 --> 0:25:09.640
<v Speaker 2>they don't always leave.

0:25:09.760 --> 0:25:12.119
<v Speaker 1>People don't always leave. There's always somebody who's going to

0:25:12.240 --> 0:25:14.919
<v Speaker 1>ride out the storm, right, Yeah. And I don't know

0:25:14.960 --> 0:25:17.000
<v Speaker 1>with the psychology there, but at least now we can

0:25:17.040 --> 0:25:20.440
<v Speaker 1>inform people further in advance and let them know where

0:25:20.440 --> 0:25:22.879
<v Speaker 1>these things are likely to go. But there's still always uncertainty,

0:25:23.160 --> 0:25:24.920
<v Speaker 1>and we'll talk about that in a minute. You don't

0:25:24.960 --> 0:25:27.520
<v Speaker 1>just have one weather prediction. You have an ensemble. You

0:25:27.520 --> 0:25:30.919
<v Speaker 1>have an envelope of predictions because you don't have perfect

0:25:31.040 --> 0:25:33.439
<v Speaker 1>data and you don't have a perfect model, and so

0:25:33.600 --> 0:25:36.000
<v Speaker 1>often what you do is you vary your data a

0:25:36.000 --> 0:25:38.399
<v Speaker 1>little bit within the uncertainties and run the model again,

0:25:38.520 --> 0:25:40.280
<v Speaker 1>and then you get a different prediction. And I'll give

0:25:40.280 --> 0:25:42.760
<v Speaker 1>you a sense of the spread of the possible outcomes.

0:25:43.240 --> 0:25:45.360
<v Speaker 1>So you might see when there's like a hurricane approaching

0:25:45.400 --> 0:25:48.520
<v Speaker 1>the coast of Florida. They have a bunch of possible trajectories.

0:25:48.560 --> 0:25:50.840
<v Speaker 1>Those are all like different runs of the weather model,

0:25:51.080 --> 0:25:54.560
<v Speaker 1>assuming different initial conditions. Because we have uncertainty, we don't

0:25:54.600 --> 0:25:55.840
<v Speaker 1>have perfect data.

0:25:55.920 --> 0:26:00.200
<v Speaker 2>I personally really enjoy learning about the uncertainty in life

0:26:00.200 --> 0:26:02.359
<v Speaker 2>in general. And whenever I look at those I have

0:26:02.440 --> 0:26:06.320
<v Speaker 2>this weird feeling of security, like, yeah, like they figured

0:26:06.320 --> 0:26:08.359
<v Speaker 2>it out and they know what the errors are. We're good,

0:26:08.600 --> 0:26:11.600
<v Speaker 2>we know what to avoid. Maybe that's maybe that's a

0:26:11.600 --> 0:26:14.000
<v Speaker 2>little bit giving it a little too much credit, but

0:26:14.000 --> 0:26:14.760
<v Speaker 2>it's still amazing.

0:26:14.880 --> 0:26:18.520
<v Speaker 1>And another really important source of uncertainty in our models

0:26:18.680 --> 0:26:21.600
<v Speaker 1>is what's happening in the ocean, like how hot is it,

0:26:21.680 --> 0:26:24.080
<v Speaker 1>how cold is it, how things circulating, all this kind

0:26:24.080 --> 0:26:27.240
<v Speaker 1>of stuff, and so we need data about the ocean.

0:26:27.240 --> 0:26:29.040
<v Speaker 1>But not a lot of people live in the ocean,

0:26:29.080 --> 0:26:31.679
<v Speaker 1>so we don't have like these automatic weather stations, but

0:26:31.720 --> 0:26:34.720
<v Speaker 1>we do have buoy's. These are like floating weather stations,

0:26:35.280 --> 0:26:38.480
<v Speaker 1>and around the world there's a couple of thousand of these,

0:26:38.560 --> 0:26:42.480
<v Speaker 1>depending on the type, that have these like temperature sensors

0:26:42.560 --> 0:26:46.080
<v Speaker 1>on the surface. But we also have this hilarious data

0:26:46.359 --> 0:26:50.040
<v Speaker 1>from what's going on deeper in the ocean that historically

0:26:50.080 --> 0:26:54.880
<v Speaker 1>has come from people on ships taking a bucket, dropping

0:26:54.920 --> 0:26:57.760
<v Speaker 1>it into the ocean, pulling it up, and then measuring

0:26:57.760 --> 0:27:00.439
<v Speaker 1>the temperature of the water. And it's like really that

0:27:00.560 --> 0:27:03.320
<v Speaker 1>lo fi. But for many years that's all we had.

0:27:03.400 --> 0:27:06.280
<v Speaker 1>We had like no other way reliably to know how

0:27:06.320 --> 0:27:09.440
<v Speaker 1>cold is it in the ocean. And this is an

0:27:09.440 --> 0:27:12.200
<v Speaker 1>example of like it's not just data. You need to

0:27:12.200 --> 0:27:15.080
<v Speaker 1>take data and interpret it and clean it and correct it.

0:27:15.520 --> 0:27:17.280
<v Speaker 1>And I spoke to an expert here, you see, I

0:27:17.440 --> 0:27:19.600
<v Speaker 1>Jane Baldwin, who told me that like you had to

0:27:19.640 --> 0:27:21.720
<v Speaker 1>correct for like how long the bucket was out of

0:27:21.720 --> 0:27:24.639
<v Speaker 1>the water before they dunked the thermometer in it, and

0:27:24.840 --> 0:27:27.400
<v Speaker 1>how Japanese ships and US ships used a different bucket

0:27:27.680 --> 0:27:29.800
<v Speaker 1>and it had different effects, and like you got to

0:27:29.880 --> 0:27:32.040
<v Speaker 1>really know, you got to be an expert and how

0:27:32.080 --> 0:27:33.879
<v Speaker 1>this data was taken and what it really means.

0:27:34.080 --> 0:27:35.560
<v Speaker 2>Yeah, So for a while I was doing some water

0:27:35.640 --> 0:27:38.240
<v Speaker 2>quality work and we had this like tube and you

0:27:38.280 --> 0:27:40.720
<v Speaker 2>would put the tube underwater and then you'd sort of

0:27:40.720 --> 0:27:44.080
<v Speaker 2>press a button and like caps would pop into place

0:27:44.119 --> 0:27:46.160
<v Speaker 2>on both sides of the tube, and then you could

0:27:46.240 --> 0:27:47.640
<v Speaker 2>lift it up and so you could get a water

0:27:47.680 --> 0:27:51.000
<v Speaker 2>sample from specifically different depths, and it was it was

0:27:51.000 --> 0:27:52.480
<v Speaker 2>always kind of fun to use that device.

0:27:52.720 --> 0:27:55.560
<v Speaker 1>Yeah, and you might think, like that's ridiculous, what a

0:27:55.840 --> 0:27:58.320
<v Speaker 1>silly system, And it's a little bit silly, but if

0:27:58.359 --> 0:28:01.680
<v Speaker 1>it's the only data you have, it's better than no data. Yeah, right,

0:28:01.920 --> 0:28:04.920
<v Speaker 1>as long as you understand the uncertainties in it. And

0:28:05.040 --> 0:28:07.600
<v Speaker 1>my friend Jane was telling me that misunderstanding this data

0:28:07.840 --> 0:28:11.040
<v Speaker 1>might be a cause for some weird pauses and global

0:28:11.080 --> 0:28:13.680
<v Speaker 1>warming trends, that it could just be like a misinterpretation

0:28:13.880 --> 0:28:17.920
<v Speaker 1>of this ship bucket dunk data.

0:28:16.960 --> 0:28:19.159
<v Speaker 2>I know, we're so moch.

0:28:20.560 --> 0:28:24.000
<v Speaker 1>These days. We have these cool robotic floats that like

0:28:24.040 --> 0:28:26.119
<v Speaker 1>float on the surface of the ocean and then dive

0:28:26.200 --> 0:28:29.639
<v Speaker 1>down up to two thousand meters measure things down in

0:28:29.720 --> 0:28:31.480
<v Speaker 1>the ocean, and then come back up and beam it

0:28:31.680 --> 0:28:35.120
<v Speaker 1>to satellites or whatever. So we're getting better obviously, yes,

0:28:35.320 --> 0:28:39.280
<v Speaker 1>But you know what's really valuable is longitudinal data. Like

0:28:39.760 --> 0:28:41.800
<v Speaker 1>you want data as far back as you can so

0:28:41.800 --> 0:28:44.640
<v Speaker 1>you can understand bigger trends. So you can't just like say, oh,

0:28:44.680 --> 0:28:47.280
<v Speaker 1>that ship bucket dunk data is ridiculous, let's ignore it.

0:28:47.280 --> 0:28:49.680
<v Speaker 1>It's the only data you have for like thirty years

0:28:49.840 --> 0:28:52.440
<v Speaker 1>and so trends in that data do tell you something

0:28:52.720 --> 0:28:53.240
<v Speaker 1>very cool.

0:28:53.600 --> 0:28:56.360
<v Speaker 2>Okay, so now we've gone down deep, how do we

0:28:56.400 --> 0:28:58.320
<v Speaker 2>get data from up high? Yeah?

0:28:58.360 --> 0:29:01.160
<v Speaker 1>Because the weather's not just at the surface, right, And

0:29:01.320 --> 0:29:03.840
<v Speaker 1>the weather folks call the surface the two meter level

0:29:03.840 --> 0:29:06.400
<v Speaker 1>because they want to measure the temperature not on the

0:29:06.480 --> 0:29:09.200
<v Speaker 1>ground literally, but like two meters up like where your

0:29:09.200 --> 0:29:11.720
<v Speaker 1>head is, essentially. But they also need to know what's

0:29:11.760 --> 0:29:14.000
<v Speaker 1>going on even further, so we take measurements in the

0:29:14.080 --> 0:29:17.959
<v Speaker 1>upper atmosphere. We use weather balloons, and these are literally

0:29:17.960 --> 0:29:20.360
<v Speaker 1>what you imagine. You put like a bunch of helium

0:29:20.440 --> 0:29:23.120
<v Speaker 1>in a balloon and you put a weather station on

0:29:23.160 --> 0:29:26.720
<v Speaker 1>it that commissure altitude, pressure, temperature, humidity, wind speed, et cetera.

0:29:27.360 --> 0:29:30.360
<v Speaker 1>And you just let it go and it rises because

0:29:30.360 --> 0:29:33.760
<v Speaker 1>helium rises, and as it goes up, the balloon expands

0:29:33.800 --> 0:29:36.080
<v Speaker 1>because the pressure in the upper atmosphere is less, and

0:29:36.160 --> 0:29:39.120
<v Speaker 1>eventually it pops and then the thing comes back down.

0:29:39.200 --> 0:29:42.600
<v Speaker 1>So these are like one time uses, right, and they

0:29:42.600 --> 0:29:44.320
<v Speaker 1>can go up like twenty kilometers.

0:29:44.680 --> 0:29:47.800
<v Speaker 2>When I visited Saint Catherine's University in Minnesota to give

0:29:47.840 --> 0:29:50.080
<v Speaker 2>a talk, they had a special day where they launched

0:29:50.120 --> 0:29:52.960
<v Speaker 2>a weather balloon, like you know for my visit and

0:29:53.600 --> 0:29:55.959
<v Speaker 2>you know, did a demonstration for all the students and

0:29:56.040 --> 0:29:57.960
<v Speaker 2>it was the coolest thing ever.

0:29:57.920 --> 0:30:01.680
<v Speaker 1>Super cool. Right, These are amazing experiments. And I know

0:30:01.760 --> 0:30:05.120
<v Speaker 1>people who do physics experiments on balloons where they like

0:30:05.160 --> 0:30:07.000
<v Speaker 1>go the Antarctic and they let up a balloon and

0:30:07.000 --> 0:30:09.120
<v Speaker 1>it floats in the atmosphere for like up to a

0:30:09.200 --> 0:30:12.000
<v Speaker 1>month or something, and like, wow, that's really brave work

0:30:12.000 --> 0:30:14.520
<v Speaker 1>because you spent like four years building this instrument and

0:30:14.520 --> 0:30:16.560
<v Speaker 1>then you're putting it on a balloon and to the

0:30:16.600 --> 0:30:20.440
<v Speaker 1>atmosphere and sometimes it's just gone, like it just disappears

0:30:20.520 --> 0:30:23.880
<v Speaker 1>and you lose your whole thesis. And this seems like

0:30:23.960 --> 0:30:26.440
<v Speaker 1>kind of bespoke, right, and it is. There's like a

0:30:26.480 --> 0:30:29.440
<v Speaker 1>couple hundred launches per day in the United States, but

0:30:29.480 --> 0:30:32.200
<v Speaker 1>it's not reliable. It's not like the place you've visited.

0:30:32.360 --> 0:30:34.680
<v Speaker 1>They do exactly the same balloon launch every single day

0:30:34.720 --> 0:30:37.120
<v Speaker 1>at the same time, right, which is the most useful

0:30:37.160 --> 0:30:40.360
<v Speaker 1>thing for a weather model. It's like reliable data and

0:30:40.400 --> 0:30:42.360
<v Speaker 1>we don't have a lot of them. But again, this

0:30:42.520 --> 0:30:44.920
<v Speaker 1>helps you probe the upper atmosphere. We don't have many

0:30:44.920 --> 0:30:47.760
<v Speaker 1>ways to measure the temperature in the upper atmosphere. This

0:30:47.800 --> 0:30:49.160
<v Speaker 1>is a really powerful one.

0:30:49.320 --> 0:30:50.640
<v Speaker 2>Do we also use planes.

0:30:51.040 --> 0:30:53.960
<v Speaker 1>We do use planes because every airplane you've been on

0:30:54.480 --> 0:30:57.760
<v Speaker 1>has really valuable information about weather because it samples from

0:30:57.840 --> 0:31:01.000
<v Speaker 1>the two meter level up to like thirty thousand feet.

0:31:01.160 --> 0:31:04.520
<v Speaker 1>An aircraft, of course have sensors to measure wind speed

0:31:04.520 --> 0:31:06.720
<v Speaker 1>and temperature and all this kind of stuff. So every

0:31:06.720 --> 0:31:10.200
<v Speaker 1>commercial airplane has these sensors, collects this data and then

0:31:10.400 --> 0:31:14.200
<v Speaker 1>sells it to the government. Noah buys this data because

0:31:14.240 --> 0:31:16.640
<v Speaker 1>there's so many flights, Like look at a map of

0:31:16.680 --> 0:31:19.320
<v Speaker 1>airplane flights for a single day in the United States.

0:31:19.360 --> 0:31:22.920
<v Speaker 1>There are so many flights they crisscross the country, and

0:31:22.960 --> 0:31:25.880
<v Speaker 1>it's incredibly valuable data. And this is usually very high

0:31:26.000 --> 0:31:28.880
<v Speaker 1>quality data because it's very important for these planes to

0:31:29.000 --> 0:31:29.840
<v Speaker 1>understand the weather.

0:31:30.160 --> 0:31:32.360
<v Speaker 2>I had no idea Noah was getting access to all

0:31:32.400 --> 0:31:33.960
<v Speaker 2>of that data. That's super cool.

0:31:34.080 --> 0:31:37.120
<v Speaker 1>It's super cool. Basically, any way you can imagine to

0:31:37.280 --> 0:31:41.520
<v Speaker 1>learn the state of the weather somewhere on Earth, somebody's

0:31:41.560 --> 0:31:43.160
<v Speaker 1>doing it, because the more data we have, the better

0:31:43.200 --> 0:31:45.840
<v Speaker 1>these models get. But then of course we can go

0:31:46.000 --> 0:31:48.800
<v Speaker 1>all the way up to space, right because there are

0:31:48.880 --> 0:31:51.560
<v Speaker 1>places where there are no automatic weather stations and there

0:31:51.600 --> 0:31:53.800
<v Speaker 1>are no buoys and there are no airplane flights, yet

0:31:53.800 --> 0:31:57.800
<v Speaker 1>they still contribute to the weather prediction in Kansas or

0:31:57.840 --> 0:32:01.720
<v Speaker 1>in Mexico City or whatever. So we have satellites, and

0:32:01.760 --> 0:32:04.240
<v Speaker 1>since about nineteen seventy nine we've had weather satellites. We

0:32:04.280 --> 0:32:07.120
<v Speaker 1>of course had satellites earlier than that, but none devoted

0:32:07.200 --> 0:32:11.480
<v Speaker 1>to like gathering weather data, and the primarily cover things

0:32:11.520 --> 0:32:14.080
<v Speaker 1>like storm systems and cloud patterns. They can tell you

0:32:14.120 --> 0:32:16.400
<v Speaker 1>where the snow is. They can also tell you like

0:32:16.440 --> 0:32:19.400
<v Speaker 1>where wildfires are, which is an important part of the weather.

0:32:20.320 --> 0:32:21.240
<v Speaker 2>Yeah, and so they.

0:32:21.120 --> 0:32:24.040
<v Speaker 1>Can't directly measure like what is the temperature in Houston

0:32:24.120 --> 0:32:27.440
<v Speaker 1>right now, but they can make indirect measurements like, for example,

0:32:27.760 --> 0:32:32.080
<v Speaker 1>they can measure the amount of infrared radiation from the surface,

0:32:32.520 --> 0:32:35.400
<v Speaker 1>and that is connected to the temperature, but it's actually

0:32:35.400 --> 0:32:38.520
<v Speaker 1>connected to the temperature of the surface, not the two

0:32:38.600 --> 0:32:41.800
<v Speaker 1>meter level. Right, So, like how hot is the blacktop

0:32:41.840 --> 0:32:44.120
<v Speaker 1>in Houston right now? That's what your satellite is telling you,

0:32:44.400 --> 0:32:46.520
<v Speaker 1>and you have to use that to infer how hot

0:32:46.600 --> 0:32:49.800
<v Speaker 1>is it two meters above the blacktop in Houston, which

0:32:49.840 --> 0:32:51.160
<v Speaker 1>is what you actually want to know.

0:32:51.600 --> 0:32:53.160
<v Speaker 2>That sounds hard, it's hard.

0:32:53.320 --> 0:32:56.280
<v Speaker 1>Yeah, exactly. And so we also don't have a lot

0:32:56.320 --> 0:32:59.640
<v Speaker 1>of satellites because they're expensive. There's something like twenty satellites

0:32:59.680 --> 0:33:03.880
<v Speaker 1>are between geostationary and polar orbits. Eight of them are

0:33:03.920 --> 0:33:06.600
<v Speaker 1>operated by Noah. But there's a bunch out there. But

0:33:06.640 --> 0:33:08.760
<v Speaker 1>my friend the climate scientist says that we might be

0:33:08.880 --> 0:33:11.320
<v Speaker 1>on the verge of having a lot more data because

0:33:11.960 --> 0:33:14.200
<v Speaker 1>launching stuff in a space is cheaper, and now we

0:33:14.240 --> 0:33:18.200
<v Speaker 1>can do like small satellites, CubeSats. These might give us

0:33:18.240 --> 0:33:21.680
<v Speaker 1>more data, not as high quality as like the dedicated

0:33:22.040 --> 0:33:26.160
<v Speaker 1>you know, super nerd designed billion dollar satellites. On the

0:33:26.240 --> 0:33:28.400
<v Speaker 1>other hand, we don't know what the future holds for

0:33:28.480 --> 0:33:32.640
<v Speaker 1>like supporting and operating these satellites. This requires money to

0:33:32.800 --> 0:33:35.800
<v Speaker 1>fund these things and have people interpreting these things. We

0:33:35.880 --> 0:33:38.200
<v Speaker 1>don't know how long the government is going to continue

0:33:38.240 --> 0:33:40.560
<v Speaker 1>to support it. They could just like unfund this stuff

0:33:40.640 --> 0:33:44.280
<v Speaker 1>or turn off weather stations. And you know it's more

0:33:44.320 --> 0:33:45.920
<v Speaker 1>than just like, oh, we turned it off for a year.

0:33:46.480 --> 0:33:50.960
<v Speaker 1>Having continuous records is super important for these models for

0:33:51.080 --> 0:33:53.560
<v Speaker 1>predicting the immediate weather, but also for the long term

0:33:53.600 --> 0:33:56.480
<v Speaker 1>climate models, which are essentially an average of the weather,

0:33:56.920 --> 0:33:59.440
<v Speaker 1>and so even turning it off briefly, could be very

0:33:59.480 --> 0:34:02.320
<v Speaker 1>damaging for our abilities to do long term predictions.

0:34:02.680 --> 0:34:04.760
<v Speaker 2>And I'm kind of blown away by the fact that

0:34:04.800 --> 0:34:07.080
<v Speaker 2>we only have twenty satellites. I guess I had assumed,

0:34:07.080 --> 0:34:09.400
<v Speaker 2>since you know, there's like five thousand satellites up there

0:34:09.480 --> 0:34:11.360
<v Speaker 2>or something. I guess most of them are dedicated to

0:34:11.440 --> 0:34:14.720
<v Speaker 2>like beaming cat videos to us from anywhere in the world.

0:34:14.800 --> 0:34:18.880
<v Speaker 2>But like weather seems so important, you know, for farmers,

0:34:19.000 --> 0:34:21.680
<v Speaker 2>for like people who are traveling, just like for everything.

0:34:21.800 --> 0:34:24.440
<v Speaker 1>Yeah, that's true, but the satellites don't give you a

0:34:24.480 --> 0:34:27.480
<v Speaker 1>direct measurement of what you're most interested in. They're essentially

0:34:27.520 --> 0:34:30.320
<v Speaker 1>like really good for filling in the gaps or places

0:34:30.360 --> 0:34:32.640
<v Speaker 1>where you have no other measurements. So yeah, it would

0:34:32.680 --> 0:34:35.160
<v Speaker 1>be great, but they're also super expensive, so you'll hear

0:34:35.160 --> 0:34:37.040
<v Speaker 1>at the end, I asked one of the climate scientists

0:34:37.080 --> 0:34:38.800
<v Speaker 1>I spoke to, like, if you had a billion dollars,

0:34:38.840 --> 0:34:41.480
<v Speaker 1>what would you spend it on? And satellites is not

0:34:41.520 --> 0:34:42.480
<v Speaker 1>their top priority.

0:34:42.840 --> 0:34:45.640
<v Speaker 2>Huh okay, all right, so maybe twenty is the right number.

0:34:47.280 --> 0:34:49.319
<v Speaker 1>So you have all these different kinds of data. You

0:34:49.360 --> 0:34:52.320
<v Speaker 1>have automatic weather stations, you have radar, you have buois,

0:34:52.400 --> 0:34:54.920
<v Speaker 1>you have ship bucket data, you have weather, balloons, aircraft,

0:34:54.960 --> 0:34:57.920
<v Speaker 1>you have satellites. What you need for your model are

0:34:57.960 --> 0:35:00.160
<v Speaker 1>the initial conditions. What you need for your model as

0:35:00.160 --> 0:35:03.000
<v Speaker 1>a set of what is the temperature and the pressure

0:35:03.040 --> 0:35:06.160
<v Speaker 1>and the humidity everywhere on the planet right now, so

0:35:06.200 --> 0:35:08.120
<v Speaker 1>that I can run it and predict it in the future.

0:35:08.800 --> 0:35:11.319
<v Speaker 1>And there's not a trivial step from like here I

0:35:11.360 --> 0:35:14.160
<v Speaker 1>have all this data to what are the initial conditions?

0:35:14.360 --> 0:35:17.600
<v Speaker 1>Because the data can disagree, right you have multiple measurements,

0:35:17.640 --> 0:35:21.040
<v Speaker 1>sometimes nearby, using different kinds of sensors. How do you

0:35:21.080 --> 0:35:23.880
<v Speaker 1>incorporate that, How do you clean this data, how do

0:35:23.920 --> 0:35:26.080
<v Speaker 1>you decide what to use? How do you merge all

0:35:26.120 --> 0:35:29.560
<v Speaker 1>of this into your best prediction? And so there's a

0:35:29.600 --> 0:35:32.160
<v Speaker 1>lot of work in this area. It's called data assimilation

0:35:32.760 --> 0:35:35.880
<v Speaker 1>of running sort of mini models fluid dynamics to do

0:35:36.000 --> 0:35:39.840
<v Speaker 1>like physics informed interpolations between the places where you don't

0:35:39.840 --> 0:35:43.600
<v Speaker 1>have measurements, and to factor in the various uncertainties from

0:35:43.640 --> 0:35:47.160
<v Speaker 1>the various different kinds of measurements. So sometimes you like

0:35:47.280 --> 0:35:49.840
<v Speaker 1>back up the model a little bit and feed in

0:35:49.920 --> 0:35:52.520
<v Speaker 1>some data and then use it to predict the current

0:35:52.520 --> 0:35:55.759
<v Speaker 1>initial conditions before you go to your full model, and

0:35:55.840 --> 0:35:58.320
<v Speaker 1>then you do what we talked about earlier, which is ensembling.

0:35:58.360 --> 0:36:01.000
<v Speaker 1>You say, well, here's my best guess for the weather,

0:36:01.080 --> 0:36:03.759
<v Speaker 1>like right now, before we even run the model. But

0:36:03.800 --> 0:36:05.839
<v Speaker 1>I'm going to make like one hundred versions of it,

0:36:05.920 --> 0:36:07.960
<v Speaker 1>and each one I'm going to tweak my assumptions a

0:36:08.040 --> 0:36:10.640
<v Speaker 1>little bit. So I get an envelope where I hope

0:36:10.719 --> 0:36:13.520
<v Speaker 1>reality somehow is described by one of these models, or

0:36:13.560 --> 0:36:15.840
<v Speaker 1>is near one of these models, or the spread in

0:36:15.880 --> 0:36:19.000
<v Speaker 1>these models describes my uncertainty in the state of the

0:36:19.040 --> 0:36:21.600
<v Speaker 1>initial conditions. We haven't even done any predictions yet. This

0:36:21.680 --> 0:36:23.960
<v Speaker 1>is just like measuring what's happening.

0:36:23.600 --> 0:36:27.080
<v Speaker 2>Now right well, and what's so stressful for me to

0:36:27.120 --> 0:36:30.160
<v Speaker 2>thinking about this is like your data are coming in constantly,

0:36:30.239 --> 0:36:31.880
<v Speaker 2>and so it's not like you do this once and

0:36:31.920 --> 0:36:33.879
<v Speaker 2>then you're like, okay, good, now we will project. It's

0:36:33.880 --> 0:36:36.359
<v Speaker 2>like every second more data are coming in. So this

0:36:36.400 --> 0:36:39.000
<v Speaker 2>has to be like a constant process that's happening over

0:36:39.040 --> 0:36:41.920
<v Speaker 2>and over again. And integrating the information into bigger models

0:36:41.920 --> 0:36:44.440
<v Speaker 2>in exactly, amazing, exactly.

0:36:44.920 --> 0:36:46.480
<v Speaker 1>And yeah, and we haven't even talked about how the

0:36:46.520 --> 0:36:47.080
<v Speaker 1>models work.

0:36:47.200 --> 0:36:49.240
<v Speaker 2>And so let's take a break and when we get back,

0:36:49.520 --> 0:37:10.719
<v Speaker 2>we'll talk about how those models work. All right, So

0:37:10.800 --> 0:37:13.640
<v Speaker 2>now we have all of this data and you've got

0:37:13.680 --> 0:37:16.480
<v Speaker 2>it into an ensemble and you sort of maybe know

0:37:16.560 --> 0:37:20.359
<v Speaker 2>what's happening right now plus some uncertainty. How do you

0:37:20.400 --> 0:37:21.960
<v Speaker 2>now predict what's going to happen next?

0:37:22.360 --> 0:37:24.719
<v Speaker 1>Yeah, so simple. You just break out your pencil and

0:37:24.760 --> 0:37:27.000
<v Speaker 1>paper and you do a bunch of strength theory calculations

0:37:27.040 --> 0:37:29.319
<v Speaker 1>and that's it. Right, it's just like physics. It into

0:37:29.320 --> 0:37:29.840
<v Speaker 1>the future.

0:37:30.320 --> 0:37:32.160
<v Speaker 2>Finally, strength theory is useful.

0:37:33.360 --> 0:37:37.160
<v Speaker 1>Yeah, unfortunately not, as we said earlier, like you can't

0:37:37.160 --> 0:37:40.399
<v Speaker 1>describe everything. You have to make assumptions about what you're

0:37:40.400 --> 0:37:43.239
<v Speaker 1>going to calculate and what you're going to simplify. Otherwise

0:37:43.280 --> 0:37:45.399
<v Speaker 1>you're never going to be able to make a prediction, right,

0:37:46.080 --> 0:37:47.520
<v Speaker 1>or your predictions are going to be done in a

0:37:47.560 --> 0:37:50.279
<v Speaker 1>thousand years for the weather that's happening in an hour,

0:37:50.320 --> 0:37:52.800
<v Speaker 1>and that's not useful. And so it's always a question

0:37:52.840 --> 0:37:56.479
<v Speaker 1>of how to judiciously make those assumptions. So the current

0:37:56.520 --> 0:37:58.759
<v Speaker 1>state of the art for weather modeling has basically two

0:37:58.840 --> 0:38:03.879
<v Speaker 1>big pieces. One is directly model the atmosphere itself as

0:38:03.920 --> 0:38:06.440
<v Speaker 1>if it's a big fluid. So you use like navea

0:38:06.480 --> 0:38:09.200
<v Speaker 1>Stokes equations and think about how it flows and how

0:38:09.200 --> 0:38:13.480
<v Speaker 1>temperature moves through it. That's the dynamical core of the model.

0:38:13.760 --> 0:38:16.960
<v Speaker 1>But there's a bunch of stuff that influences the atmosphere

0:38:17.120 --> 0:38:21.200
<v Speaker 1>that you don't explicitly include in the model. The clouds,

0:38:21.239 --> 0:38:25.319
<v Speaker 1>the convection, the ocean, the radiation, the surface temperature, all

0:38:25.360 --> 0:38:28.479
<v Speaker 1>this kind of stuff. Your model doesn't explicitly include that stuff.

0:38:28.520 --> 0:38:30.680
<v Speaker 1>We don't have like a complete model of the ocean

0:38:31.120 --> 0:38:34.560
<v Speaker 1>or the clouds, etc. And so we have like various

0:38:34.560 --> 0:38:38.560
<v Speaker 1>inputs to this core piece that they call parameterizations that

0:38:38.680 --> 0:38:42.240
<v Speaker 1>like capture the big picture effects of all these pieces

0:38:42.239 --> 0:38:45.560
<v Speaker 1>that are not included directly in our model but are

0:38:45.640 --> 0:38:46.760
<v Speaker 1>influencing us.

0:38:47.320 --> 0:38:50.520
<v Speaker 2>So I feel like this is a question where you

0:38:50.520 --> 0:38:52.480
<v Speaker 2>think to yourself, am I about to ask a really

0:38:52.520 --> 0:38:54.560
<v Speaker 2>stupid question? But I'm going to move forward because that's

0:38:54.560 --> 0:38:58.880
<v Speaker 2>my job in this podcast. The atmosphere is not a

0:38:58.920 --> 0:39:04.840
<v Speaker 2>fluid though, right, So like guy, am, so, what why

0:39:04.920 --> 0:39:07.120
<v Speaker 2>are we doing? Are we modeling it as a fluid

0:39:07.200 --> 0:39:10.040
<v Speaker 2>because we just can't model it as something else because

0:39:10.040 --> 0:39:15.600
<v Speaker 2>it's too complicated and fluids are a simplification or Daniel,

0:39:15.640 --> 0:39:17.480
<v Speaker 2>I don't think the atmosphere is a fluid.

0:39:18.320 --> 0:39:20.040
<v Speaker 1>Well, it depends on what you mean by a fluid,

0:39:20.600 --> 0:39:22.760
<v Speaker 1>and you know, when it comes to like how things

0:39:22.800 --> 0:39:26.600
<v Speaker 1>flow and pressure, et cetera, the fluid dynamic equations do

0:39:26.719 --> 0:39:31.600
<v Speaker 1>describe the atmosphere. And so you know, fluid doesn't mean liquid, right,

0:39:31.719 --> 0:39:35.000
<v Speaker 1>Fluid is about how things flow and move. Right. So,

0:39:35.080 --> 0:39:38.360
<v Speaker 1>for example, like the mantle of the Earth is a fluid.

0:39:38.760 --> 0:39:42.560
<v Speaker 1>It flows. It's not a liquid, right, It's this weird

0:39:43.000 --> 0:39:45.920
<v Speaker 1>solidy kind of state and it moves, but it also flows,

0:39:45.960 --> 0:39:48.280
<v Speaker 1>and so you can describe it and it has convection.

0:39:48.440 --> 0:39:51.759
<v Speaker 1>You can describe it with fluid equations. And so the

0:39:51.840 --> 0:39:55.440
<v Speaker 1>Navi or Stokes equations are these famous equations that describe

0:39:55.440 --> 0:39:58.760
<v Speaker 1>fluid dynamics and they're pretty good at modeling the atmosphere.

0:39:58.760 --> 0:40:01.280
<v Speaker 1>They're not perfect, right, They're not perfect, but they're pretty

0:40:01.280 --> 0:40:03.239
<v Speaker 1>good at it. So, yeah, I think fluid is not

0:40:03.320 --> 0:40:05.160
<v Speaker 1>a liquid. It's just things that flow.

0:40:05.400 --> 0:40:08.799
<v Speaker 2>Okay, in my head, fluid is synonymous with liquid. And

0:40:08.840 --> 0:40:11.480
<v Speaker 2>so I have learned something today that will probably help

0:40:11.520 --> 0:40:13.319
<v Speaker 2>me not look silly in the future. That's great.

0:40:13.360 --> 0:40:15.840
<v Speaker 1>No, it was a great question. And so this is

0:40:15.880 --> 0:40:18.560
<v Speaker 1>the big picture. You have the dynamical core, and then

0:40:18.600 --> 0:40:21.080
<v Speaker 1>you have these parameterizations and we'll dig into that and

0:40:21.120 --> 0:40:23.200
<v Speaker 1>we'll describe sort of the US approach to it. But

0:40:23.239 --> 0:40:27.080
<v Speaker 1>there are three sort of major weather communities. There's the US,

0:40:27.120 --> 0:40:31.880
<v Speaker 1>the UK, and the Japanese, and they have slightly different approaches,

0:40:32.239 --> 0:40:35.280
<v Speaker 1>which is good because you know, different predictions can crosscheck

0:40:35.320 --> 0:40:38.200
<v Speaker 1>each other. But then some people think it's bad because hey,

0:40:38.239 --> 0:40:40.120
<v Speaker 1>let's pool all of our resources and make one big

0:40:40.160 --> 0:40:42.400
<v Speaker 1>global model, and that's awesome, but then you only have

0:40:42.440 --> 0:40:44.480
<v Speaker 1>the one and you're not sure. Maybe it's all wrong.

0:40:45.000 --> 0:40:46.799
<v Speaker 1>There's a lot of debate about, you know, how to

0:40:46.840 --> 0:40:49.520
<v Speaker 1>deal with global questions and global resources.

0:40:49.560 --> 0:40:50.440
<v Speaker 2>But who's the best.

0:40:53.040 --> 0:40:55.120
<v Speaker 1>Oh, I'll give you a ranking at the end. Okay,

0:40:55.160 --> 0:40:58.440
<v Speaker 1>all right, So the dynamical core, Right, think of the atmosphere.

0:40:58.600 --> 0:41:01.480
<v Speaker 1>We're going to treat the atmosphere basically like a spherical cow. Right,

0:41:01.680 --> 0:41:05.319
<v Speaker 1>It is a spherical fluid, right, the atmosphere. Yeah, it's

0:41:05.400 --> 0:41:09.680
<v Speaker 1>a thin shell around the Earth, and you know the

0:41:09.680 --> 0:41:13.440
<v Speaker 1>temperature and the pressure, and then you can describe how

0:41:13.480 --> 0:41:15.600
<v Speaker 1>it's going to flow, how the temperature and pressure are

0:41:15.600 --> 0:41:19.600
<v Speaker 1>going to change using the Navier Stokes equations. So Navia

0:41:19.640 --> 0:41:23.840
<v Speaker 1>Stokes is a set of really gnarly equations. They're nonlinear

0:41:24.160 --> 0:41:28.560
<v Speaker 1>partial differential equations. A differential equation is one where like

0:41:29.080 --> 0:41:33.040
<v Speaker 1>the value depends on how quickly it's changing. For example,

0:41:33.080 --> 0:41:36.680
<v Speaker 1>like antecology, you have differential equations that describe like predator

0:41:36.680 --> 0:41:39.680
<v Speaker 1>and prey. Right, these two things are coupled, and so

0:41:39.719 --> 0:41:43.160
<v Speaker 1>these are nonlinear partial differential equations, which means like that

0:41:43.280 --> 0:41:46.360
<v Speaker 1>depends on things squared or cubed. All that to say,

0:41:46.480 --> 0:41:49.799
<v Speaker 1>they're very, very difficult to solve. In fact, differential equations

0:41:49.840 --> 0:41:51.520
<v Speaker 1>in general are hard to solve. If you've taken a

0:41:51.560 --> 0:41:55.000
<v Speaker 1>differential equations class, it's basically like differential equations are not

0:41:55.080 --> 0:41:58.840
<v Speaker 1>solvable except for these four examples that we have answers

0:41:58.880 --> 0:42:01.160
<v Speaker 1>to and we know how to solve them, and so

0:42:01.200 --> 0:42:03.319
<v Speaker 1>you just got to memorize those. It's a little bit

0:42:03.360 --> 0:42:03.960
<v Speaker 1>like chemistry.

0:42:04.000 --> 0:42:05.000
<v Speaker 2>I gotta say, oh no.

0:42:05.080 --> 0:42:09.080
<v Speaker 1>It's mostly unsolved, right. And the Navias Stokes equations we've

0:42:09.080 --> 0:42:11.160
<v Speaker 1>known about them for like two hundred years that were

0:42:11.200 --> 0:42:14.239
<v Speaker 1>initially developed to try to answer these questions about like

0:42:14.280 --> 0:42:17.280
<v Speaker 1>how do things flow and how does momentum and mass

0:42:17.280 --> 0:42:21.640
<v Speaker 1>flow through pipes, et cetera. Essentially, people took Newton's second

0:42:21.719 --> 0:42:25.279
<v Speaker 1>law ethicals MA and applied it to fluids and then

0:42:25.400 --> 0:42:29.160
<v Speaker 1>added terms for like stress and pressure and viscosity. And

0:42:29.280 --> 0:42:31.319
<v Speaker 1>it's like a real triumph that we can describe this

0:42:31.400 --> 0:42:35.120
<v Speaker 1>at all. But calculationally it's a real bear. You can't

0:42:35.160 --> 0:42:38.400
<v Speaker 1>like sit down and derive a solution and say, here's

0:42:38.440 --> 0:42:40.640
<v Speaker 1>my pressure and temperature. Let me crunch it through the

0:42:40.719 --> 0:42:43.560
<v Speaker 1>Naviastokes equation. It's going to give me a formula. It's

0:42:43.640 --> 0:42:47.120
<v Speaker 1>all numerical approximations, which means it takes a lot of

0:42:47.120 --> 0:42:50.160
<v Speaker 1>computing to go from now to one second from now

0:42:50.280 --> 0:42:54.440
<v Speaker 1>or two seconds from now, and that computing means approximating things.

0:42:54.480 --> 0:42:59.080
<v Speaker 1>You're like doing numerical derivatives instead of exact analytical derivatives.

0:42:59.320 --> 0:43:02.200
<v Speaker 2>Okay, so some of that got pretty complicated, But what

0:43:02.320 --> 0:43:03.719
<v Speaker 2>I guess what I want to know is when this

0:43:03.760 --> 0:43:06.120
<v Speaker 2>is all done, I feel like, if we are trying

0:43:06.160 --> 0:43:08.600
<v Speaker 2>to model fluids, does this just tell us that, like,

0:43:09.040 --> 0:43:12.080
<v Speaker 2>the wind is now over here going this fast but

0:43:12.120 --> 0:43:14.440
<v Speaker 2>before it was over there? And how many are we

0:43:14.480 --> 0:43:16.319
<v Speaker 2>going to get to like how you get from that

0:43:16.440 --> 0:43:18.800
<v Speaker 2>to like and it's raining, Because that seems like a

0:43:18.840 --> 0:43:22.120
<v Speaker 2>different problem sort of than how fluid is moving around.

0:43:22.560 --> 0:43:24.000
<v Speaker 1>Yeah, so there's a couple of things to know there.

0:43:24.000 --> 0:43:26.120
<v Speaker 1>You're exactly right. It takes the current conditions and tries

0:43:26.120 --> 0:43:29.080
<v Speaker 1>to predict the future conditions. And those conditions are pressure

0:43:29.160 --> 0:43:33.520
<v Speaker 1>and temperature, wind speed, humidity, right, these kinds of things.

0:43:33.920 --> 0:43:37.680
<v Speaker 1>But because we're solving this numerically, we can't solve it everywhere.

0:43:38.239 --> 0:43:40.799
<v Speaker 1>If you have a formula and analytics description you can

0:43:40.800 --> 0:43:43.600
<v Speaker 1>write down, for like, where is my ball as I've

0:43:43.640 --> 0:43:45.120
<v Speaker 1>thrown it? I can write that down on a piece

0:43:45.120 --> 0:43:46.680
<v Speaker 1>of paper a formula. I can tell you where the

0:43:46.680 --> 0:43:49.080
<v Speaker 1>ball is at any point in time. You ask me

0:43:49.200 --> 0:43:52.080
<v Speaker 1>any point literally any value of T, I could plug

0:43:52.120 --> 0:43:54.759
<v Speaker 1>it into my formula give you an answer. But if

0:43:54.760 --> 0:43:57.440
<v Speaker 1>I don't have a formula, that's called an analytics description.

0:43:58.000 --> 0:44:00.160
<v Speaker 1>If all I have is a numerical estimate, then I've

0:44:00.200 --> 0:44:02.440
<v Speaker 1>made a grid. I've said I'm going to sample it

0:44:02.680 --> 0:44:04.839
<v Speaker 1>at time one time, two time, three time four, I'm

0:44:04.840 --> 0:44:06.960
<v Speaker 1>going to make an estimate of those times, and it

0:44:07.040 --> 0:44:10.000
<v Speaker 1>don't have an answer everywhere. And that's the situation we

0:44:10.040 --> 0:44:11.840
<v Speaker 1>have with weathers that they put a grid on the

0:44:11.840 --> 0:44:16.040
<v Speaker 1>planet and they estimate what's going to be the weather, temperature,

0:44:16.120 --> 0:44:19.799
<v Speaker 1>et cetera, in a grid of points, not everywhere over

0:44:19.840 --> 0:44:22.120
<v Speaker 1>the planet. And you might think, oh, I bet that

0:44:22.160 --> 0:44:24.680
<v Speaker 1>grid's pretty small, right, maybe they measure down to the

0:44:24.719 --> 0:44:28.120
<v Speaker 1>centimeter or something. No, the grid sizes are like ten

0:44:28.239 --> 0:44:29.520
<v Speaker 1>kilometer cubes.

0:44:29.800 --> 0:44:31.720
<v Speaker 2>What, Yes, that's too big.

0:44:31.800 --> 0:44:35.640
<v Speaker 1>It's too big, right. They are averaging the temperature and

0:44:35.640 --> 0:44:39.920
<v Speaker 1>the humidity over cubes of atmosphere ten kilometers on a side,

0:44:40.200 --> 0:44:42.920
<v Speaker 1>it's crazy and I think that's way too big. On

0:44:42.960 --> 0:44:45.279
<v Speaker 1>the other hand, that's still a lot of cubes, right,

0:44:45.400 --> 0:44:48.400
<v Speaker 1>Like the atmosphere is a lot of ten kilometer sized cubes.

0:44:48.920 --> 0:44:52.840
<v Speaker 1>And then the time steps are tens of minutes, right,

0:44:52.920 --> 0:44:55.319
<v Speaker 1>And this is awesome that we can even do this.

0:44:55.560 --> 0:44:58.640
<v Speaker 1>It requires massive supercomputers. We'll talk about it in a minute.

0:44:59.000 --> 0:45:01.080
<v Speaker 1>But the problem is that it ignores a lot of

0:45:01.080 --> 0:45:04.399
<v Speaker 1>little details like how big is a cloud? Usually they're

0:45:04.480 --> 0:45:08.160
<v Speaker 1>like a kilometer or less. And so you're missing out

0:45:08.200 --> 0:45:11.040
<v Speaker 1>on a lot of stuff by making your grid. Anything

0:45:11.040 --> 0:45:15.319
<v Speaker 1>that happens that's subgrid. That's crucial and important, but it's

0:45:15.320 --> 0:45:17.359
<v Speaker 1>small than the size of your grid is not being

0:45:17.400 --> 0:45:20.600
<v Speaker 1>described by your model. But your question was like, is

0:45:20.640 --> 0:45:23.160
<v Speaker 1>this directly outputting? Like, hey, it's going to rain on

0:45:23.239 --> 0:45:26.719
<v Speaker 1>Kelly's picnic. In a sense, yes, the direct outputs are

0:45:26.719 --> 0:45:30.320
<v Speaker 1>things like temperature, pressure, humidity, and those are enough to

0:45:30.360 --> 0:45:32.799
<v Speaker 1>tell you like, okay, it's going to rain because the

0:45:32.880 --> 0:45:35.680
<v Speaker 1>pressure and humidity are above some threshold or whatever. So

0:45:35.719 --> 0:45:39.239
<v Speaker 1>it's not directly outputting like three centimeters of snow. There's

0:45:39.239 --> 0:45:41.400
<v Speaker 1>another step you have to take after that, but it

0:45:41.440 --> 0:45:43.480
<v Speaker 1>feeds into that. So those are the inputs you need

0:45:43.520 --> 0:45:45.560
<v Speaker 1>to the next step, which says how much snow is

0:45:45.600 --> 0:45:46.040
<v Speaker 1>going to fall?

0:45:46.239 --> 0:45:47.360
<v Speaker 2>Okay, So let me see if I can do a

0:45:47.360 --> 0:45:50.560
<v Speaker 2>super simplified version of this. You get all of the

0:45:50.640 --> 0:45:53.160
<v Speaker 2>data that you have about a square in the grid,

0:45:53.840 --> 0:45:55.759
<v Speaker 2>and you do the best job you can to sort

0:45:55.760 --> 0:45:58.200
<v Speaker 2>of summarize it and ensemble it, and then you put

0:45:58.239 --> 0:46:02.520
<v Speaker 2>it in the model the runs through the equations. Than

0:46:02.600 --> 0:46:07.640
<v Speaker 2>does the information from the surrounding grids feed into your

0:46:07.680 --> 0:46:09.680
<v Speaker 2>grid as well, because you would, okay, because you would

0:46:09.680 --> 0:46:13.319
<v Speaker 2>expect there to be similarities between closely related squares in

0:46:13.320 --> 0:46:13.720
<v Speaker 2>the grid.

0:46:13.920 --> 0:46:15.640
<v Speaker 1>Yeah, you can't solve one grid at a time. You

0:46:15.640 --> 0:46:18.359
<v Speaker 1>have to solve all the grids. To grids touch each

0:46:18.360 --> 0:46:21.560
<v Speaker 1>other and influence each other and wind flows right right,

0:46:21.600 --> 0:46:25.319
<v Speaker 1>And that's why Siberia affects Manhattan over time because you've

0:46:25.360 --> 0:46:28.200
<v Speaker 1>propagated these things from grid cell to grid cell.

0:46:28.239 --> 0:46:32.840
<v Speaker 2>Absolutely, So does Siberia have bigger grid cells or just

0:46:32.960 --> 0:46:35.480
<v Speaker 2>the same number of small grid cells each with poorer

0:46:35.560 --> 0:46:36.279
<v Speaker 2>data in them.

0:46:36.560 --> 0:46:40.120
<v Speaker 1>Yeah, great questions. So some of these models are adaptive, right,

0:46:40.160 --> 0:46:42.880
<v Speaker 1>they have bigger grid cells where we have more uncertainty,

0:46:42.920 --> 0:46:46.200
<v Speaker 1>and smaller we have more data. The most precise ones

0:46:46.280 --> 0:46:49.680
<v Speaker 1>are the UK supercomputers. They go down to two kilometers

0:46:50.080 --> 0:46:52.840
<v Speaker 1>in some cases. Some of them are like fixed grids,

0:46:52.840 --> 0:46:55.400
<v Speaker 1>and some of them are adaptive exactly. It depends a

0:46:55.440 --> 0:46:58.000
<v Speaker 1>little bit on the model. But you know, there's lots

0:46:58.040 --> 0:47:00.680
<v Speaker 1>of details that are not described here, and these are

0:47:00.680 --> 0:47:04.840
<v Speaker 1>called the parameterizations, like especially subgrid stuff and exchanges with

0:47:04.920 --> 0:47:07.399
<v Speaker 1>other parts of the system. They're not just the fluid.

0:47:07.600 --> 0:47:10.720
<v Speaker 1>And one important thing are the clouds. Like you cannot

0:47:10.760 --> 0:47:13.799
<v Speaker 1>model every individual cloud because clouds are smaller than your

0:47:13.800 --> 0:47:15.759
<v Speaker 1>grid size. We do not have the compute to do that.

0:47:15.800 --> 0:47:19.080
<v Speaker 1>People have tried, and you can like do dedicated runs

0:47:19.120 --> 0:47:22.120
<v Speaker 1>on subsets to try to resolve clouds, but then you

0:47:22.160 --> 0:47:24.480
<v Speaker 1>don't have enough computing to do like ensembles. So you

0:47:24.520 --> 0:47:27.240
<v Speaker 1>can be like one prediction you're like, well, here's a prediction,

0:47:27.360 --> 0:47:29.279
<v Speaker 1>but I don't know what the uncertainties are on it

0:47:29.320 --> 0:47:32.160
<v Speaker 1>at all. And so instead what you tend to do

0:47:32.560 --> 0:47:36.840
<v Speaker 1>is parameterize the bulk outcomes, you know, the vapor, the clouds,

0:47:36.840 --> 0:47:39.839
<v Speaker 1>the liquid, the ice, the rain, the snow, etc. The condensation,

0:47:40.520 --> 0:47:42.760
<v Speaker 1>all this kind of stuff. You try to like grab

0:47:42.880 --> 0:47:46.040
<v Speaker 1>all that average over what's happening in that grid cell

0:47:46.040 --> 0:47:49.000
<v Speaker 1>and use that to inform your naveor Stokes equation. So

0:47:49.360 --> 0:47:52.680
<v Speaker 1>things you're not explicitly modeling, you're sort of like averaging

0:47:52.760 --> 0:47:55.719
<v Speaker 1>over You're losing all the details and saying like, well,

0:47:55.760 --> 0:47:57.640
<v Speaker 1>on average, this is going to be the effect of

0:47:57.719 --> 0:47:59.279
<v Speaker 1>clouds on my grid cell.

0:48:00.000 --> 0:48:01.960
<v Speaker 2>Do you think that as Oh, well, I was going

0:48:02.040 --> 0:48:04.000
<v Speaker 2>to say, do you think that as we continue to

0:48:04.040 --> 0:48:06.840
<v Speaker 2>have more and more computing power and more and more supercomputers,

0:48:06.840 --> 0:48:09.359
<v Speaker 2>at some point we'll be doing better here? But we

0:48:09.360 --> 0:48:13.160
<v Speaker 2>were just talking about how More's law. We've maybe hit

0:48:13.239 --> 0:48:16.120
<v Speaker 2>the end of that. So are we like, is this

0:48:16.160 --> 0:48:17.600
<v Speaker 2>as good as wherever we're going to get at it?

0:48:17.640 --> 0:48:19.719
<v Speaker 2>This is probably an end of the podcast question, but

0:48:19.760 --> 0:48:20.880
<v Speaker 2>I'm thinking it right now.

0:48:22.239 --> 0:48:24.920
<v Speaker 1>No, I think that there's lots of possibilities for making

0:48:24.960 --> 0:48:28.239
<v Speaker 1>this faster and more efficient, and not just wait till

0:48:28.280 --> 0:48:31.200
<v Speaker 1>computers get faster. Okay, there's definitely clever ideas and we'll

0:48:31.239 --> 0:48:33.840
<v Speaker 1>get there. Yeah, But there are lots of parts of

0:48:33.880 --> 0:48:36.600
<v Speaker 1>the weather that are not directly described in the dynamical core,

0:48:36.719 --> 0:48:39.480
<v Speaker 1>and not just the clouds, but also things like convection,

0:48:39.680 --> 0:48:44.359
<v Speaker 1>like vertical transport of heat. You know, especially there is

0:48:44.480 --> 0:48:49.160
<v Speaker 1>complex boundary mixing near the surface, like the lowest kilometer

0:48:49.239 --> 0:48:51.439
<v Speaker 1>or so of the atmosphere, where you have like heat

0:48:51.480 --> 0:48:55.279
<v Speaker 1>from the surface and turbulent momentum exchanges as wind is

0:48:55.320 --> 0:48:58.480
<v Speaker 1>like hitting mountains and stuff. These things. You can't model

0:48:58.520 --> 0:49:01.880
<v Speaker 1>all of those details, and so you have like parameterization

0:49:02.080 --> 0:49:05.640
<v Speaker 1>schemes that model the turbulence and the boundary level mixings.

0:49:06.160 --> 0:49:10.120
<v Speaker 1>There's radiation from the surface also, right that changes from

0:49:10.160 --> 0:49:14.239
<v Speaker 1>day to night. You have models of vegetation and snow

0:49:15.080 --> 0:49:17.920
<v Speaker 1>how those things couple. But then the biggest one is

0:49:17.960 --> 0:49:21.280
<v Speaker 1>the ocean. Right, Like we would love for our models

0:49:21.320 --> 0:49:25.640
<v Speaker 1>to include also a Navio Stoke simulation of the whole ocean, right,

0:49:25.920 --> 0:49:27.560
<v Speaker 1>might as well do that because the ocean it plays

0:49:27.600 --> 0:49:29.640
<v Speaker 1>a big role. But we don't have the compute for

0:49:29.680 --> 0:49:32.480
<v Speaker 1>that at all, So we just like use a slab

0:49:32.520 --> 0:49:35.240
<v Speaker 1>ocean model. We just say, let's just assume the ocean

0:49:35.320 --> 0:49:38.239
<v Speaker 1>is like simple, and we have a certain temperature, and

0:49:38.280 --> 0:49:42.560
<v Speaker 1>we assume like how the energy transfers from the boundaries,

0:49:43.000 --> 0:49:46.480
<v Speaker 1>and it's really quite simplified. But that's we're just limited, right.

0:49:46.520 --> 0:49:48.440
<v Speaker 1>We don't have great data in the ocean, and we

0:49:48.480 --> 0:49:50.759
<v Speaker 1>don't have the compute to also model the ocean as

0:49:50.800 --> 0:49:54.360
<v Speaker 1>well as the atmosphere. So places where we don't do

0:49:54.400 --> 0:49:57.239
<v Speaker 1>our best approximation, which is like Navia Stokes equations of

0:49:57.239 --> 0:50:00.959
<v Speaker 1>the atmosphere, we have simplified versions, which are called parmetization. Says,

0:50:01.000 --> 0:50:03.759
<v Speaker 1>feed in to the core. But in the end you

0:50:03.800 --> 0:50:06.120
<v Speaker 1>got to take it to the computers. And this is

0:50:06.160 --> 0:50:09.799
<v Speaker 1>why we have like massive supercomputers to make weather predictions.

0:50:10.120 --> 0:50:13.040
<v Speaker 1>So Noah in the US has a couple of really

0:50:13.080 --> 0:50:16.279
<v Speaker 1>big facilities. They're called Dogwood and Cactus. One of them

0:50:16.320 --> 0:50:16.600
<v Speaker 1>is in.

0:50:16.600 --> 0:50:18.560
<v Speaker 2>Virginia, You're welcome, everyone.

0:50:18.280 --> 0:50:21.720
<v Speaker 1>And one of them is in Arizona, and they're huge,

0:50:21.880 --> 0:50:26.640
<v Speaker 1>amazing computers. Those two have like twelve point one petaflops.

0:50:26.960 --> 0:50:27.839
<v Speaker 2>You made that word up.

0:50:28.160 --> 0:50:31.759
<v Speaker 1>It sounds like a made up word. Peta means quadrillion

0:50:31.880 --> 0:50:35.759
<v Speaker 1>and flops are floating point operations. So you know it

0:50:35.800 --> 0:50:39.440
<v Speaker 1>takes the computer time to add like three point nine

0:50:39.480 --> 0:50:42.799
<v Speaker 1>to one to fourteen point four two and floating point

0:50:42.880 --> 0:50:45.360
<v Speaker 1>numbers those numbers with a dot in them, right, not

0:50:45.520 --> 0:50:50.279
<v Speaker 1>integers are more computationally expensive to add or subtract. And

0:50:50.320 --> 0:50:52.120
<v Speaker 1>that's what most of these models do. They're like, add

0:50:52.120 --> 0:50:54.480
<v Speaker 1>this number, multiply by this, and so this is like

0:50:54.600 --> 0:50:57.319
<v Speaker 1>the way you measure the speed of a computer. And

0:50:57.400 --> 0:51:01.280
<v Speaker 1>so these computers can each do twelve point one quadrillion

0:51:01.560 --> 0:51:03.880
<v Speaker 1>floating point operations per second.

0:51:04.080 --> 0:51:04.360
<v Speaker 2>Wow.

0:51:04.440 --> 0:51:06.839
<v Speaker 1>Right, imagine the guys back in the nineteen twenties, they're

0:51:06.880 --> 0:51:09.640
<v Speaker 1>like adding two numbers. It probably takes them a minute, right,

0:51:09.719 --> 0:51:13.040
<v Speaker 1>or they're super good, takes them twenty seconds. The computer

0:51:13.160 --> 0:51:18.480
<v Speaker 1>does twelve quadrillion a piece per second. Right. So together

0:51:18.760 --> 0:51:22.160
<v Speaker 1>with all of their computers, Noah has about fifty petaflops

0:51:22.520 --> 0:51:25.000
<v Speaker 1>and that's what it uses to run its model. And

0:51:25.040 --> 0:51:27.719
<v Speaker 1>so that's the state of the art. In the United States.

0:51:28.360 --> 0:51:32.080
<v Speaker 1>The Europeans have a couple of computers. Is one really

0:51:32.080 --> 0:51:35.720
<v Speaker 1>big one in Bologna called Bull Sequanya and has about

0:51:35.719 --> 0:51:40.279
<v Speaker 1>thirty petaflops. But the biggest, most powerful weather computer in

0:51:40.320 --> 0:51:43.120
<v Speaker 1>the world is in the UK. It's at the Met

0:51:43.160 --> 0:51:47.120
<v Speaker 1>Office and it's built by Microsoft and has sixty petaflops.

0:51:47.239 --> 0:51:49.520
<v Speaker 1>And this is why the UK has some of the

0:51:49.520 --> 0:51:52.320
<v Speaker 1>best weather prediction in the world because they have the

0:51:52.360 --> 0:51:55.759
<v Speaker 1>biggest computer. They beat us. Yeah exactly, they just spent

0:51:55.840 --> 0:51:58.359
<v Speaker 1>more money. They bought more computer. This is literally like

0:51:58.640 --> 0:51:59.800
<v Speaker 1>money equals computing.

0:52:00.719 --> 0:52:02.000
<v Speaker 2>Tea drinking bastards.

0:52:02.400 --> 0:52:06.399
<v Speaker 1>Good day. Yeah, well, you know, they got tricky weather

0:52:06.480 --> 0:52:09.400
<v Speaker 1>over there, and so they need it. It's an island

0:52:09.400 --> 0:52:13.319
<v Speaker 1>after yet guys and the Japanese. The Japanese have a

0:52:13.360 --> 0:52:16.439
<v Speaker 1>big investment in weather prediction computers. Also, this one called

0:52:16.480 --> 0:52:19.960
<v Speaker 1>Prime HBC. It has thirty one petaflops. So these are

0:52:19.960 --> 0:52:23.359
<v Speaker 1>really powerful devices and they run these huge models. And

0:52:23.480 --> 0:52:25.799
<v Speaker 1>you know, think about what the model does. It predicts

0:52:26.080 --> 0:52:30.080
<v Speaker 1>the state of the atmosphere on these pretty chunky grids.

0:52:30.120 --> 0:52:32.319
<v Speaker 1>But it's still it's a huge amount of data, like

0:52:32.440 --> 0:52:35.880
<v Speaker 1>every few minutes, every ten kilometers. My friend Jane was

0:52:35.880 --> 0:52:38.880
<v Speaker 1>telling me that sometimes the data is so big that

0:52:39.000 --> 0:52:41.280
<v Speaker 1>you just throw it away. You run it, you get

0:52:41.280 --> 0:52:43.640
<v Speaker 1>like a summary number, but you can't keep all of

0:52:43.640 --> 0:52:45.560
<v Speaker 1>the data because it would just like fill up all

0:52:45.600 --> 0:52:48.400
<v Speaker 1>of the hard drives. Everywhere. And this is familiar for

0:52:48.440 --> 0:52:50.399
<v Speaker 1>me because like at the LHC, we also we run

0:52:50.440 --> 0:52:54.040
<v Speaker 1>these experiments every twenty five danoseconds. We throw away most

0:52:54.040 --> 0:52:56.479
<v Speaker 1>of the data from that because it would just fill

0:52:56.560 --> 0:52:59.400
<v Speaker 1>up all of our storage. And they're in a similar situation.

0:52:59.440 --> 0:53:01.480
<v Speaker 1>They produce more data than they can store.

0:53:01.960 --> 0:53:07.279
<v Speaker 2>So are these facilities where the Navier Stokes equations are

0:53:07.320 --> 0:53:11.200
<v Speaker 2>being run or are these facilities where you have the

0:53:11.239 --> 0:53:14.319
<v Speaker 2>output from each grid and now you are translating that

0:53:14.400 --> 0:53:16.440
<v Speaker 2>into information about where the rain is falling?

0:53:17.200 --> 0:53:21.640
<v Speaker 1>Both? Yeah, okay, So these programs do the data similation,

0:53:22.000 --> 0:53:24.360
<v Speaker 1>come up with the current initial conditions, and then also

0:53:24.640 --> 0:53:28.000
<v Speaker 1>run the model forward to make those predictions, and from

0:53:28.040 --> 0:53:32.560
<v Speaker 1>that glean things like weather details, snowfall, et cetera. And

0:53:32.600 --> 0:53:34.439
<v Speaker 1>so what you're getting on your phone, what you're hearing

0:53:34.440 --> 0:53:37.400
<v Speaker 1>on TV is not just like what Jane, your local forecaster,

0:53:37.560 --> 0:53:42.480
<v Speaker 1>came up with. She's relying heavily on these central predictions

0:53:42.800 --> 0:53:47.160
<v Speaker 1>from major resources. Right, So, for example, if worldwide governments

0:53:47.200 --> 0:53:50.160
<v Speaker 1>decide we don't need these computers anymore, we don't need

0:53:50.200 --> 0:53:52.760
<v Speaker 1>these satellites, it's not like you could be like, that's cool,

0:53:53.000 --> 0:53:55.560
<v Speaker 1>I got my local weather forecaster I don't need you.

0:53:55.560 --> 0:53:58.719
<v Speaker 1>No your local weather forecaster is getting that information from

0:53:58.800 --> 0:54:01.600
<v Speaker 1>these big models that are being run by the government.

0:54:02.080 --> 0:54:06.359
<v Speaker 2>Oh wow, yeah, and did Noah get cuts recently? I'm

0:54:06.360 --> 0:54:07.160
<v Speaker 2>going to bet they did.

0:54:07.400 --> 0:54:09.120
<v Speaker 1>There were some talk about cuts. I don't know how

0:54:09.160 --> 0:54:11.440
<v Speaker 1>much of that is going through. It's all kind of scary.

0:54:12.160 --> 0:54:12.840
<v Speaker 1>It's hard to know.

0:54:13.200 --> 0:54:15.839
<v Speaker 2>Yeah, okay, all right, we won't get into that. Moving on.

0:54:16.800 --> 0:54:21.160
<v Speaker 1>But amazingly, currently we can pretty accurately predict the weather

0:54:21.320 --> 0:54:24.040
<v Speaker 1>five to six days in the future, you know, and

0:54:24.080 --> 0:54:26.680
<v Speaker 1>you mostly remember when the weather prediction is wrong. You

0:54:26.719 --> 0:54:29.600
<v Speaker 1>mostly don't realize that most of the time it's right. Yeah,

0:54:29.640 --> 0:54:30.840
<v Speaker 1>you know, it tells you it's going to rain, it

0:54:30.840 --> 0:54:32.840
<v Speaker 1>tells you it's going to be study. It's mostly correct.

0:54:32.920 --> 0:54:36.399
<v Speaker 1>It's amazing, but you know, there's still challenges. Things are

0:54:36.440 --> 0:54:40.400
<v Speaker 1>not perfect. One of the biggest challenge is just incomplete information.

0:54:41.000 --> 0:54:43.719
<v Speaker 1>You know, we don't have sensors in enough places, and

0:54:43.760 --> 0:54:48.240
<v Speaker 1>we don't have enough sensors, and sometimes this data availability changes,

0:54:48.280 --> 0:54:50.560
<v Speaker 1>you know, things go offline or come online. Now your

0:54:50.560 --> 0:54:53.200
<v Speaker 1>model has to compensate for that. I don't have the data.

0:54:53.320 --> 0:54:55.480
<v Speaker 1>Do I assume it's similar to the past. Do I

0:54:55.520 --> 0:54:58.200
<v Speaker 1>try to ignore that kind of data. It's not easy

0:54:58.280 --> 0:55:01.520
<v Speaker 1>to be running a model if the puts are constantly changing.

0:55:01.760 --> 0:55:03.279
<v Speaker 2>The bucket had a hole in it, So now you

0:55:03.320 --> 0:55:06.960
<v Speaker 2>don't have good bucket data exactly exactly.

0:55:07.080 --> 0:55:08.600
<v Speaker 1>They got a new kind of bucket. You don't know

0:55:08.680 --> 0:55:11.279
<v Speaker 1>how to calibrate it. I spoke to John Martin, he's

0:55:11.280 --> 0:55:13.960
<v Speaker 1>a professor of meteorology, and he said that this might

0:55:14.000 --> 0:55:16.759
<v Speaker 1>be the biggest challenge is how to combine the data

0:55:16.880 --> 0:55:20.760
<v Speaker 1>to make a high quality initial state. That's one challenge.

0:55:20.800 --> 0:55:24.760
<v Speaker 1>The other are these subgrid parameterizations. Can we develop better

0:55:24.840 --> 0:55:28.040
<v Speaker 1>models for turbulent flow at the boundaries or for latent

0:55:28.120 --> 0:55:32.120
<v Speaker 1>he's released back into the environment. And another limiting factor

0:55:32.200 --> 0:55:35.520
<v Speaker 1>is just the computing cost. More computes, more GPUs from

0:55:35.600 --> 0:55:40.040
<v Speaker 1>Nvidia means smaller grids, which means the effect of these approximations,

0:55:40.040 --> 0:55:45.279
<v Speaker 1>these parameterizations is less. Another continuing challenge are rare and

0:55:45.400 --> 0:55:49.920
<v Speaker 1>extreme events, like we're pretty good at predicting the bigger picture,

0:55:50.120 --> 0:55:51.600
<v Speaker 1>like is it going to be sunny here, is it

0:55:51.600 --> 0:55:55.560
<v Speaker 1>going to be rainy here? But like small, rare extreme events,

0:55:55.560 --> 0:55:58.719
<v Speaker 1>like there's a tornado right here, that's more challenging because

0:55:58.719 --> 0:56:01.600
<v Speaker 1>they depends in detail well on things that happen within

0:56:01.680 --> 0:56:05.160
<v Speaker 1>the grid that we're averaging over. And so there's a

0:56:05.200 --> 0:56:07.879
<v Speaker 1>lot of work being done right now. One thing we're

0:56:07.880 --> 0:56:10.080
<v Speaker 1>hoping to do is like, let's reduce the grid size,

0:56:10.160 --> 0:56:14.560
<v Speaker 1>get more computing, more accurate. Right. But another really promising

0:56:14.640 --> 0:56:18.759
<v Speaker 1>error of research is using machine learning. Oh, there's this

0:56:18.960 --> 0:56:21.879
<v Speaker 1>movement in many fields of science to use machine learning

0:56:21.880 --> 0:56:25.239
<v Speaker 1>to make predictions by essentially skipping the physics. Like, the

0:56:25.280 --> 0:56:27.520
<v Speaker 1>physics is hard, it takes a lot of time to

0:56:27.560 --> 0:56:30.839
<v Speaker 1>push the initial conditions through these equations. In the end

0:56:31.120 --> 0:56:34.640
<v Speaker 1>you have an input and an output. And the idea is, well,

0:56:34.680 --> 0:56:38.320
<v Speaker 1>can we train machine learning, not a chatbot, not LMS,

0:56:39.000 --> 0:56:43.160
<v Speaker 1>it's AI, but it's not LMS to map the initial

0:56:43.160 --> 0:56:46.200
<v Speaker 1>conditions to the output because in the end it's just

0:56:46.239 --> 0:56:49.200
<v Speaker 1>a mapping and one could learn it. And so we

0:56:49.280 --> 0:56:52.480
<v Speaker 1>have these machine learning models that are simple functions that

0:56:52.560 --> 0:56:55.040
<v Speaker 1>take the input and give you the output, and they

0:56:55.040 --> 0:56:57.360
<v Speaker 1>don't have the physics encoded in them, but they learn

0:56:57.480 --> 0:57:00.319
<v Speaker 1>from the simulations, they learn the patterns, they learn what

0:57:00.400 --> 0:57:03.440
<v Speaker 1>the rules are implicitly, and so you don't have to

0:57:03.480 --> 0:57:07.160
<v Speaker 1>go through all the detailed calculations. So this can dramatically

0:57:07.200 --> 0:57:09.840
<v Speaker 1>speed up your predictions. We use these the large handroom

0:57:09.840 --> 0:57:12.160
<v Speaker 1>collider all the time so that we don't have to,

0:57:12.360 --> 0:57:15.279
<v Speaker 1>for example, model every single particle that might hit the

0:57:15.320 --> 0:57:18.200
<v Speaker 1>detector and create another particle and another particle. We can

0:57:18.320 --> 0:57:21.360
<v Speaker 1>learn to predict the final thing we're interested in and

0:57:21.400 --> 0:57:24.240
<v Speaker 1>to sort of leapfrog over all the tiny details.

0:57:24.600 --> 0:57:27.400
<v Speaker 2>And his machine learning being used right now for weather predictions,

0:57:27.480 --> 0:57:29.160
<v Speaker 2>or they're just starting to work on how you would

0:57:29.160 --> 0:57:29.360
<v Speaker 2>do that.

0:57:29.920 --> 0:57:32.240
<v Speaker 1>They're using that now. There's sort of experimental. But there's

0:57:32.240 --> 0:57:34.360
<v Speaker 1>a guy here at you see Irvine, Mike Pritchard, who

0:57:34.400 --> 0:57:36.680
<v Speaker 1>is an expert in this kind of stuff, and it's

0:57:36.800 --> 0:57:40.560
<v Speaker 1>very powerful, absolutely cool. Yeah. So I asked John Martin,

0:57:40.600 --> 0:57:43.480
<v Speaker 1>if I give you a billion dollars to improve weather predictions,

0:57:43.560 --> 0:57:45.800
<v Speaker 1>what would you do, And he said he would spend

0:57:45.800 --> 0:57:48.800
<v Speaker 1>a billion dollars on ocean probes, like he wanted a

0:57:48.840 --> 0:57:52.120
<v Speaker 1>more substantial understanding of how water is circulating in the

0:57:52.160 --> 0:57:55.400
<v Speaker 1>ocean and temperature in the ocean and how that's all working.

0:57:55.400 --> 0:57:58.160
<v Speaker 1>Because his suspicion was like, we're right next to this

0:57:58.240 --> 0:58:00.800
<v Speaker 1>other big fluid that's affecting our temperaatereure, and we don't

0:58:00.800 --> 0:58:03.000
<v Speaker 1>have much enough data about it. If we just knew

0:58:03.320 --> 0:58:06.520
<v Speaker 1>more about the ocean, and this just highlights like how

0:58:06.680 --> 0:58:09.400
<v Speaker 1>little information we have. It's not just a question of

0:58:09.440 --> 0:58:11.840
<v Speaker 1>like puzzling out the rules of the universe, but just

0:58:11.880 --> 0:58:15.640
<v Speaker 1>like knowing what's happening. If we had more data everywhere

0:58:15.960 --> 0:58:19.720
<v Speaker 1>about temperature, pressure, about cosmic rays, we would just learn

0:58:19.800 --> 0:58:22.760
<v Speaker 1>so much about the universe. And we have so few

0:58:22.800 --> 0:58:25.480
<v Speaker 1>ways to probe. But we're really just like taking the

0:58:25.560 --> 0:58:29.720
<v Speaker 1>tiniest teaspoon out of this massive river of data and

0:58:29.760 --> 0:58:32.240
<v Speaker 1>trying to use that to understand the whole river. It's crazy.

0:58:32.480 --> 0:58:34.360
<v Speaker 2>How good do you think weather prediction would have to

0:58:34.360 --> 0:58:36.880
<v Speaker 2>be before people stopped complaining about weather prediction?

0:58:37.800 --> 0:58:40.440
<v Speaker 1>I asked John that question, and his prediction was, quote,

0:58:40.560 --> 0:58:44.040
<v Speaker 1>the complaining will never stop amazing. I think that, you know,

0:58:44.080 --> 0:58:46.960
<v Speaker 1>weather prediction has improved a lot over the last few decades.

0:58:47.720 --> 0:58:49.760
<v Speaker 1>It used to be you couldn't get any reliable prediction

0:58:49.840 --> 0:58:52.200
<v Speaker 1>more than a day in advance. Now five six days,

0:58:52.240 --> 0:58:55.600
<v Speaker 1>it's pretty reliable. But people expect that and they get

0:58:55.680 --> 0:58:57.680
<v Speaker 1>used to it, and they're like, what, you didn't predict

0:58:57.680 --> 0:59:00.360
<v Speaker 1>the weather or my ski trip in two weeks? I'm you,

0:59:01.000 --> 0:59:03.240
<v Speaker 1>And so yeah, the complaining will never stop because we

0:59:03.280 --> 0:59:07.080
<v Speaker 1>always just get used to the level of technological prowess

0:59:07.720 --> 0:59:10.920
<v Speaker 1>that we've had, and so people want more because it's

0:59:10.960 --> 0:59:13.680
<v Speaker 1>so important and it's a hard problem. There's so much

0:59:13.720 --> 0:59:17.240
<v Speaker 1>physics here, there's instrumental science, there's so many different kinds

0:59:17.280 --> 0:59:19.720
<v Speaker 1>of science at interface with each other. It's really an

0:59:19.720 --> 0:59:22.160
<v Speaker 1>exciting field. And let me throw a special thanks to

0:59:22.240 --> 0:59:24.920
<v Speaker 1>Professor Jane Baldwin here you see I who told me

0:59:24.960 --> 0:59:27.520
<v Speaker 1>a lot about weather predictions, and Professor John Martin at

0:59:27.520 --> 0:59:30.240
<v Speaker 1>Wisconsin who answered a lot of naive questions of mine.

0:59:30.280 --> 0:59:31.000
<v Speaker 1>Thanks to both of you.

0:59:31.200 --> 0:59:33.880
<v Speaker 2>Thank you community. All right, see you all next time.

0:59:33.920 --> 0:59:35.440
<v Speaker 2>I hope the weather is nice where you are.

0:59:35.920 --> 0:59:46.400
<v Speaker 5>It always will be nice where I am.

0:59:46.520 --> 0:59:50.360
<v Speaker 2>Daniel and Kelly's Extraordinary Universe is produced by iHeartRadio. We

0:59:50.400 --> 0:59:51.800
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