WEBVTT - Cruel Summer

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<v Speaker 1>Brought to you by Toyota. Let's go places. Hello, I

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<v Speaker 1>am Lauren Vogue. Bam, this is Forward Thinking Jonathan stricklind

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<v Speaker 1>is going to cut him in just a moment, but

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<v Speaker 1>we had a quick addendum to the following episode. It's

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<v Speaker 1>going to be about climate change and future oriented. Though

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<v Speaker 1>we maybe we could not have predicted that when we

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<v Speaker 1>recorded this on September sevent or so, that the Intergovernmental

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<v Speaker 1>Panel on Climate Change was going to release a new

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<v Speaker 1>report just about a week later. Now this new report

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<v Speaker 1>is very much in line with the trends that we're

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<v Speaker 1>going to talk about in this episode. But in case

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<v Speaker 1>you would like the updated facts and figures, I'm going

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<v Speaker 1>to write a blog post about that. It is going

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<v Speaker 1>to go up slightly after this episode airs, so go

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<v Speaker 1>over to fw thinking dot com to check that out

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<v Speaker 1>and stay tuned. Thank you. Welcome to Forward Thinking Taylor

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<v Speaker 1>to one and welcome to Forward Thinking, the podcast that

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<v Speaker 1>looks at the future and says it's a cool, cruel

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<v Speaker 1>summer leading me here on my own. I'm Jonathan Strickland,

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<v Speaker 1>I'm Lauren Vogue Obama, and I'm Joe McCormick. And that

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<v Speaker 1>sound of disapproval comes from Lauren, who is shaking her

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<v Speaker 1>head at me. Today we're going to talk about climate change.

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<v Speaker 1>What is climate change? What's global warming? Are they the

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<v Speaker 1>same thing? What's what's the deal? Yeah? Climate change? So

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<v Speaker 1>I saw a movie about it, um, like convenient truth.

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<v Speaker 1>You know. It was called The Day After Tomorrow. Oh

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<v Speaker 1>that movie, right, it came out a few years back.

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<v Speaker 1>I don't know if you saw it, but it had

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<v Speaker 1>it had some very attractive actors in it, uh, and

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<v Speaker 1>they fought against the evil villain of climate change. Basically,

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<v Speaker 1>what I learned from it was that climate change creates

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<v Speaker 1>uh intelligent anthropogenic ice that chases you down hallways or

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<v Speaker 1>or Jill down hallways. Right. It's really had it in

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<v Speaker 1>for him. Um that that that everything happens in like

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<v Speaker 1>I don't remember. It was like it looked like it

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<v Speaker 1>was like an hour. My favorite part of that movie

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<v Speaker 1>is watching characters running from the cold front as it's

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<v Speaker 1>passing over and turning things instantly into ice, and just

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<v Speaker 1>barely slipping inside a library and shutting the door to

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<v Speaker 1>keep the cold front out people. It's like when people

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<v Speaker 1>run away from an explosion, right and they're able to

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<v Speaker 1>outrun it. Yeah, it made me think that there was

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<v Speaker 1>going to be a knock at the door, and then

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<v Speaker 1>you just hear cold front like, no, don't get it. Yeah,

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<v Speaker 1>but yeah, everything I learned from this movie, is this

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<v Speaker 1>all correct? Let's just say that the film takes some

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<v Speaker 1>liberties with science. Oh okay, so then climate change, global warming,

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<v Speaker 1>these things aren't really happening. See, as it turns out,

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<v Speaker 1>there's actually a middle ground between the movie The Day

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<v Speaker 1>After Tomorrow and the complete denial that climate change and

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<v Speaker 1>global warming are a thing. Well, I like to uh

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<v Speaker 1>listen to what scientists have to say. Let's so, well,

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<v Speaker 1>first let's let's define some terms, right, okay, because I mean,

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<v Speaker 1>obviously we're gonna be talking a lot about global warming

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<v Speaker 1>and climate change. And one thing that we notice is

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<v Speaker 1>that maybe in popular science reporting and in general amongst

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<v Speaker 1>the public, these two terms tend to be confused or

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<v Speaker 1>sometimes used interchangeably, and that's not exactly correct. Yeah. It

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<v Speaker 1>turns out that if you talk to scientists, how they

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<v Speaker 1>use these terms is that global warming refers more often

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<v Speaker 1>specifically to the increase in the mean surface temperature of

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<v Speaker 1>the Earth. It's caused specifically by human human emissions. Right,

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<v Speaker 1>that this recent trend we're talking about, right, right, whereas

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<v Speaker 1>climate change refers to both global warming and everything else

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<v Speaker 1>that causes the climate to change over a given period

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<v Speaker 1>of time a k a. Usually a very long period

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<v Speaker 1>of time, right, Yeah, So you can think of global

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<v Speaker 1>warming is sort of like a specific phenomenon and climate

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<v Speaker 1>change is like that phenomenon plus all of its effects. Right.

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<v Speaker 1>And then on top of that, you also have the

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<v Speaker 1>scientific literature that tends to use these these two different

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<v Speaker 1>terms in very specific contexts. So if you were to

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<v Speaker 1>actually read a paper, one paper might be about global warming,

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<v Speaker 1>another one might be about climate change, and those two

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<v Speaker 1>terms are not meant to be interchanged at all, Whereas,

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<v Speaker 1>like I said, with some of the in the media,

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<v Speaker 1>sometimes they just get tossed around without people really being

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<v Speaker 1>very aware of what right it's. It may be that

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<v Speaker 1>someone is unaware of the difference or that they're just misspeaking,

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<v Speaker 1>but at any rate, there does seem to be this

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<v Speaker 1>this idea that the two terms are used, or that

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<v Speaker 1>one was used before and now the other one is preferred.

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<v Speaker 1>Like there there's a there's a perception and misperception. As

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<v Speaker 1>it turns out that global warming was the term that

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<v Speaker 1>everyone was using in the eighties, and then once everyone

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<v Speaker 1>figured out, oh wait, no, no, no, it's not global warming,

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<v Speaker 1>it's climate change. It's switched. That's not actually true. Those

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<v Speaker 1>two terms are still used pretty much just as frequently

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<v Speaker 1>as they were before, but they're in that very specific context.

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<v Speaker 1>So it all depends upon the context of whatever research

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<v Speaker 1>you're reading as to which term will be used. But

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<v Speaker 1>the difference is actually pretty intuitive. They're what they sound like.

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<v Speaker 1>Global warming refers to the warming. Climate change refers to

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<v Speaker 1>the overall climate. But wait a minute, Wait a minute, Joe, Joe,

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<v Speaker 1>I'm I'm confused. I mean, yesterday was not as hot

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<v Speaker 1>as two days ago, which in turn was hotter than

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<v Speaker 1>the day before that, and a few days before that

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<v Speaker 1>was less hot. I don't see how this climate thing

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<v Speaker 1>is affecting me. Am I making a mistake. You might

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<v Speaker 1>be making a mistake. Um, For one thing, here, your

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<v Speaker 1>sample size is one. It's you. Yeah, I'm a very

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<v Speaker 1>reliable narrator. It's also a very small sample of days. Okay, sure, sure.

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<v Speaker 1>So to understand global trends in climate, we need to

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<v Speaker 1>step back and look at really massive systems and averages

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<v Speaker 1>across a lot of different time scales and geographical location, right,

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<v Speaker 1>because climate is global, whereas weather, which is what you're

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<v Speaker 1>talking about, is is local. Yes, yes, weather is local.

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<v Speaker 1>And weather is something that we usually refer to in

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<v Speaker 1>terms of, well we can it can be as short

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<v Speaker 1>as a few minutes and as long as a few months,

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<v Speaker 1>but that tends to be what we're referring to when

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<v Speaker 1>we talk about weather. Climate is a much longer term, uh,

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<v Speaker 1>subject matter. And like you said, Joe, we're talking about

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<v Speaker 1>global scale with climate, not just Jonathan in the metropolitan

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<v Speaker 1>Atlanta area over the course of the last two weeks.

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<v Speaker 1>So that that but that's one of those other things

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<v Speaker 1>that we see get confused often as the idea between

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<v Speaker 1>climate and weather, and in fact, that can cause confusion

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<v Speaker 1>when you're discussing things like climate change and global global warming,

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<v Speaker 1>because if someone says, yeah, but you know, this summer

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<v Speaker 1>just didn't seem as hot as last summer, it's it's

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<v Speaker 1>a total different scale than what we're talking about. Basically,

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<v Speaker 1>if you can make small talk about it in an

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<v Speaker 1>elevator with someone that you don't know politely, then its weather,

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<v Speaker 1>not climate. That's a good rubric. Did you did you

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<v Speaker 1>notice that the glacial ice is two less over the

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<v Speaker 1>last twenty years than it was over the last hundred

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<v Speaker 1>and twenty years. I see, I have different elevator experiences

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<v Speaker 1>that you clearly do. Okay, Jonathan's elevator experiences are just primo.

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<v Speaker 1>You gotta ask him about them sometimes, Okay. Uh, So

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<v Speaker 1>let's talk about temperature, okay, because clearly the central feature

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<v Speaker 1>of climate change is this idea that the temperature is increasing?

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<v Speaker 1>Number one? Is that true? And number two? How do

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<v Speaker 1>we know? Uh? It is true? And we know because

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<v Speaker 1>we take measurements and we examine them. The acceleration of

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<v Speaker 1>heating that we've seen over the last century is far

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<v Speaker 1>greater than what we can account for using the natural

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<v Speaker 1>cycles of the Earth. So, in other words, we're seeing

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<v Speaker 1>a more rapid acceleration in heating than we would normally

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<v Speaker 1>see if, in fact, human intervention had not been a factor.

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<v Speaker 1>So what kind of differences are we talking about in

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<v Speaker 1>recent years? Is it like a hundred degrees hotter? Well? So, okay,

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<v Speaker 1>So over the past five thousand years or so, global

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<v Speaker 1>temperatures rose a total of four to seven degrees celsius,

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<v Speaker 1>depending on you know, the absolute liability of our data,

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<v Speaker 1>And um, that's that's what like seven point two to

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<v Speaker 1>twelve point six degrees fahrenheit. I didn't just make that

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<v Speaker 1>up off the top of my head. I wrote it

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<v Speaker 1>down just to have a saying. Um, but uh, in

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<v Speaker 1>the past century alone, um temperatures rose point seven degrees celsius.

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<v Speaker 1>That's one point to six degrees fahrenheit, which is about

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<v Speaker 1>ten times faster than the average rate of ice age

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<v Speaker 1>recovery warming. And on top of that, projection suggests that

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<v Speaker 1>by the end of the twenty first century, the temperature

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<v Speaker 1>will continue to arise between two degrees celsius and six

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<v Speaker 1>degrees celsius. That's kind of a range that's given. Uh.

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<v Speaker 1>You know, six obviously would be the worst case scenario.

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<v Speaker 1>But even if we were to quote unquote fix all

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<v Speaker 1>the problems, and we'll talk about fixing the problems in

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<v Speaker 1>the future podcast, but if we were to fix them,

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<v Speaker 1>we would still experience, uh, an increase in temperature because

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<v Speaker 1>there's a lag between addressing the problem and having the

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<v Speaker 1>problem actually resolve in any way, right, UM, And all

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<v Speaker 1>of us data is based on a whole lot of

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<v Speaker 1>figures that we are collecting about um. You know, the

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<v Speaker 1>the amount of radiation we're getting from the sun and

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<v Speaker 1>everything unhouse gases that are present in the atmosphere, uh,

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<v Speaker 1>everything from the cloud cover that can be a factor.

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<v Speaker 1>In fact, there's some people who suggest that uh, through

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<v Speaker 1>increased evaporation due to heat heating of the oceans, that

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<v Speaker 1>that will increase the cloud cover and that's that would

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<v Speaker 1>actually help help cool the earth. Uh. I'm not I'm

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<v Speaker 1>not a sold on that particular, on that particular interpretation.

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<v Speaker 1>Got I've got a bunch of information on that one.

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<v Speaker 1>The general answers, We're not sure yet, but we'll talk

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<v Speaker 1>about that in a future podcast. But but but now,

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<v Speaker 1>the kind of data that we collect is about the aerosols,

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<v Speaker 1>the particles in our atmosphere, atmosphere gases, the ocean surface

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<v Speaker 1>temperature changes, global sea level, extent of ocean, ice, plant growth, rainfall,

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<v Speaker 1>cloud structure, uh, ground temperature, snow depth records. I mean,

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<v Speaker 1>like all of this data is going into the way

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<v Speaker 1>that scientists define these estimates of global warming and UM.

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<v Speaker 1>When they take all of this data from natural events

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<v Speaker 1>and from human created events, they try to kind of

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<v Speaker 1>reverse engineer the temperature ranges that we've seen and UM,

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<v Speaker 1>the models that they create bork around nineteen fifty. If

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<v Speaker 1>you don't take into account human intervention. Right, So in

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<v Speaker 1>other words, when you if you were to say this

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<v Speaker 1>is only based this is just part of the Earth's

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<v Speaker 1>natural cycle, like this is exactly the same sort of

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<v Speaker 1>thing that's happened in the past. You can't account for

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<v Speaker 1>the amount of change we're seeing now in the in

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<v Speaker 1>the time span. That's the really important part is that

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<v Speaker 1>these are changes that we would see happen to the

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<v Speaker 1>Earth in a natural warming trend, but we would see

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<v Speaker 1>them stretched out over a much longer time span than

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<v Speaker 1>half a century. Okay, so the Earth is definitely warming recently,

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<v Speaker 1>and basically nobody denies this, right, And dude, that's well, well, basically,

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<v Speaker 1>I think most people who look at the science say no,

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<v Speaker 1>there's there's plenty of evidence here, pretty straightforward data. It's

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<v Speaker 1>just getting hotter. It's not like a question about that,

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<v Speaker 1>although there are people who will say that, no, it's

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<v Speaker 1>not getting warmer because look, the Arctic ice has recovered

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<v Speaker 1>from ice recovered compared to Therefore the worth the Earth

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<v Speaker 1>is not warming, or it's warming at a slower pace,

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<v Speaker 1>or it's declining. Again, a single year of data isn't

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<v Speaker 1>enough to base a trend upon, and the trends that

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<v Speaker 1>we are talking about have lasted since um at least

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<v Speaker 1>nine Yeah. So, so there are people who do deny

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<v Speaker 1>that the Earth is warming, but they are not as

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<v Speaker 1>numerous as those who deny the larger question of climate

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<v Speaker 1>change in general. Okay, Um, so the Earth is warming,

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<v Speaker 1>what's causing it? Well, that's where not some more the

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<v Speaker 1>argument comes in? Right? Yeah, so have y'all heard of

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<v Speaker 1>the greenhouse effect? Wait? What have you ever been inside

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<v Speaker 1>a greenhouse? I have? Or have you ever been inside

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<v Speaker 1>just a parked car out in the sunlight. My wife

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<v Speaker 1>leaves me there all the time. When into the story,

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<v Speaker 1>I beg her to crack a window, she just takes

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<v Speaker 1>the key out and it's power windows. So I'm just stuck. Seriously,

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<v Speaker 1>people don't leave your animals. No, no, no, it's bad,

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<v Speaker 1>very bad. Um. And it's bad because in a way

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<v Speaker 1>of the green house effect. Okay, so the greenhouse effect

0:13:03.760 --> 0:13:07.680
<v Speaker 1>happens when, um, there is sort of a differential in

0:13:07.760 --> 0:13:11.560
<v Speaker 1>the two way transportation of energy through a medium. So

0:13:11.880 --> 0:13:14.640
<v Speaker 1>it happens in a greenhouse when the sunlight comes through

0:13:14.640 --> 0:13:18.520
<v Speaker 1>the glass comes in and allows that that UV radiation,

0:13:18.640 --> 0:13:21.360
<v Speaker 1>all the sun's energy to come through one way, but

0:13:21.400 --> 0:13:26.480
<v Speaker 1>then it traps heat inside. Um. The Earth actually works

0:13:26.480 --> 0:13:28.960
<v Speaker 1>in a very similar way in the atmosphere, right. Yeah,

0:13:29.000 --> 0:13:32.160
<v Speaker 1>the atmosphere is kind of like the glass in a greenhouse.

0:13:32.520 --> 0:13:35.120
<v Speaker 1>And this is totally natural and in fact, if it

0:13:35.200 --> 0:13:37.920
<v Speaker 1>didn't happen, there wouldn't really be life as we know it. No,

0:13:38.040 --> 0:13:42.040
<v Speaker 1>if it didn't happen, the Earth would basically be the moon. Um. Right.

0:13:42.120 --> 0:13:45.320
<v Speaker 1>The the the heat trapped by the atmosphere keeps the

0:13:45.360 --> 0:13:48.559
<v Speaker 1>Earth at a habitable temperature. Right, that's exactly right. And

0:13:48.800 --> 0:13:51.440
<v Speaker 1>um So the greenhouse effect is not a bad thing,

0:13:52.000 --> 0:13:55.560
<v Speaker 1>and it's caused by multiple types of gases in the atmosphere.

0:13:55.720 --> 0:13:58.959
<v Speaker 1>Um So, the biggest one actually is water vapor, right,

0:13:59.040 --> 0:14:01.520
<v Speaker 1>that one. That one ends up trapping heat at an

0:14:01.559 --> 0:14:04.800
<v Speaker 1>efficiency far greater than that of other greenhouse gasses. Yeah,

0:14:04.840 --> 0:14:10.880
<v Speaker 1>so water vapor, UM, cloud particles, carbon dioxide uh CFCs

0:14:10.920 --> 0:14:15.520
<v Speaker 1>so chlorofluoro carbons um in O two I believe, and

0:14:15.760 --> 0:14:20.040
<v Speaker 1>methane gases like this. Um. They hover up in the

0:14:20.040 --> 0:14:23.040
<v Speaker 1>atmosphere and what happens is the sunlight passes through them

0:14:23.040 --> 0:14:25.760
<v Speaker 1>on the way to the Earth, bringing energy with it.

0:14:26.120 --> 0:14:29.480
<v Speaker 1>That sunlight hits the Earth's crust and gets absorbed, and

0:14:29.520 --> 0:14:32.600
<v Speaker 1>when it radiates back upward it is heat. That heat

0:14:32.680 --> 0:14:36.200
<v Speaker 1>gets trapped under those gases and does not pass backward

0:14:36.320 --> 0:14:38.480
<v Speaker 1>out of the Earth, so we get sort of a

0:14:38.560 --> 0:14:42.400
<v Speaker 1>net gain of heat on the planet. Um. A certain

0:14:42.400 --> 0:14:44.760
<v Speaker 1>amount of this of this, like we've said, is good

0:14:44.920 --> 0:14:49.680
<v Speaker 1>because it allows us to not freeze to death. But um,

0:14:49.720 --> 0:14:54.800
<v Speaker 1>if you have too much greenhouse effect from an overconcentration

0:14:54.880 --> 0:14:58.320
<v Speaker 1>of greenhouse gasses, you can trap more heat than you're

0:14:58.400 --> 0:15:02.440
<v Speaker 1>used to, which is is what most scientists agree is

0:15:02.480 --> 0:15:05.680
<v Speaker 1>going on right now to cause this heating trend we've

0:15:05.720 --> 0:15:09.200
<v Speaker 1>observed recently, which in turn is driving climate change. So

0:15:09.440 --> 0:15:13.760
<v Speaker 1>what can we do about this? Well, we can't really

0:15:13.800 --> 0:15:16.880
<v Speaker 1>mess with water vapor much because there's a water cycle

0:15:16.920 --> 0:15:19.440
<v Speaker 1>on Earth that we need. It turns out water is

0:15:19.480 --> 0:15:22.280
<v Speaker 1>pretty important. Rain is kind of critical, so we don't

0:15:22.280 --> 0:15:24.400
<v Speaker 1>want to mess with the water. Um. But there are

0:15:24.400 --> 0:15:28.360
<v Speaker 1>these other gases that are non condensing gases as opposed

0:15:28.400 --> 0:15:31.480
<v Speaker 1>to water. Because water vapor condenses, it forms clouds. These

0:15:31.480 --> 0:15:36.920
<v Speaker 1>non condensing gases, and mainly most scientists degree carbon dioxide

0:15:37.360 --> 0:15:40.280
<v Speaker 1>are responsible for a huge part of the trend in

0:15:40.320 --> 0:15:44.640
<v Speaker 1>global warming. And the reason this is happening is because

0:15:44.840 --> 0:15:48.600
<v Speaker 1>we've increased the amount of carbon dioxide in our atmosphere

0:15:48.600 --> 0:15:51.520
<v Speaker 1>since the Industrial Revolution. So what you can do is

0:15:51.560 --> 0:15:54.400
<v Speaker 1>you can you can drill a cylinder of ancient ice

0:15:54.480 --> 0:15:56.920
<v Speaker 1>out of a glacier and pull that up and look

0:15:56.960 --> 0:15:59.480
<v Speaker 1>at it. And it turns out when ice freezes, it

0:15:59.560 --> 0:16:02.440
<v Speaker 1>traps little air bubbles in it, and those air bubbles

0:16:02.440 --> 0:16:04.920
<v Speaker 1>are like little time capsules of what the atmosphere was

0:16:05.000 --> 0:16:08.320
<v Speaker 1>like in throughout history. Yeah, and so we can look

0:16:08.320 --> 0:16:10.760
<v Speaker 1>at these, and this is one type of evidence we

0:16:10.800 --> 0:16:15.040
<v Speaker 1>have for the historical presence of carbon dioxide in the atmosphere.

0:16:15.640 --> 0:16:18.160
<v Speaker 1>What these ice cores tend to show is that pre

0:16:18.200 --> 0:16:21.720
<v Speaker 1>industrial air had about two hundred and eighty parts per

0:16:21.760 --> 0:16:26.880
<v Speaker 1>million of C O two um. This year we hit

0:16:27.080 --> 0:16:34.840
<v Speaker 1>four hundred parts per million, so we uh, not nearly doubled,

0:16:34.840 --> 0:16:37.880
<v Speaker 1>but we but half a yeah, yeah that's true, half

0:16:37.880 --> 0:16:42.280
<v Speaker 1>again as much. And that's a big deal earlier. And

0:16:42.360 --> 0:16:46.960
<v Speaker 1>so there are questions about exactly how much carbon needs

0:16:47.000 --> 0:16:50.800
<v Speaker 1>to be in the atmosphere to cause a significant increase

0:16:50.840 --> 0:16:54.440
<v Speaker 1>in the greenhouse effect. Um, what I've heard some people

0:16:54.520 --> 0:16:56.480
<v Speaker 1>say is like, well, we really need to get down

0:16:56.520 --> 0:16:58.840
<v Speaker 1>to three d and fifty parts per million for a

0:16:58.880 --> 0:17:03.280
<v Speaker 1>stable climate. UM four hundred was sort of like some

0:17:03.320 --> 0:17:05.720
<v Speaker 1>people have said, that's like a sort of turning point

0:17:05.920 --> 0:17:09.840
<v Speaker 1>or a point of stability that that really cannot be exceeded.

0:17:10.240 --> 0:17:12.399
<v Speaker 1>And now it's like, well, we already hit that, and

0:17:12.720 --> 0:17:16.160
<v Speaker 1>so there's sort of this smoothing scale of what can

0:17:16.160 --> 0:17:21.800
<v Speaker 1>feasibly be tolerated UM. The point is that is that

0:17:21.960 --> 0:17:25.199
<v Speaker 1>there's a correlation between the amount of carbon in the

0:17:25.240 --> 0:17:30.280
<v Speaker 1>atmosphere and the and the temperature the or the sorry

0:17:30.320 --> 0:17:32.359
<v Speaker 1>the climate. So you can look at look at this.

0:17:32.400 --> 0:17:34.960
<v Speaker 1>I think you mentioned earlier that these ice cores, for example,

0:17:35.000 --> 0:17:38.439
<v Speaker 1>you can look at dates um in the strata of

0:17:38.520 --> 0:17:41.680
<v Speaker 1>the ice and it turns out that times when there

0:17:41.760 --> 0:17:44.960
<v Speaker 1>was less carbon in the atmosphere or less carbon dioxide,

0:17:45.520 --> 0:17:50.040
<v Speaker 1>there were ice ages or colder periods, and time when

0:17:50.080 --> 0:17:54.360
<v Speaker 1>the carbon dioxide and the atmosphere spiked there were warmer periods,

0:17:54.400 --> 0:17:57.320
<v Speaker 1>just like we're seeing now. And you can argue that

0:17:57.320 --> 0:18:00.480
<v Speaker 1>part of this is due to U volcanic activity. Even today,

0:18:00.520 --> 0:18:02.439
<v Speaker 1>there have been a couple of large volcanoes that have

0:18:02.560 --> 0:18:06.280
<v Speaker 1>erupted UM over the past few decades that have caused

0:18:06.440 --> 0:18:09.080
<v Speaker 1>a significant amount of carbon dioxide to be released into

0:18:09.080 --> 0:18:11.159
<v Speaker 1>the air. They also tend to release a lot of

0:18:11.480 --> 0:18:16.000
<v Speaker 1>sulfur dioxide, which tends to lower it has a cooling

0:18:16.040 --> 0:18:19.679
<v Speaker 1>effect from cloud creation. Yeah. From what I've read, it

0:18:19.760 --> 0:18:22.160
<v Speaker 1>seems to be that they think that the volcanoes are

0:18:22.200 --> 0:18:26.199
<v Speaker 1>not a significant contributor, certainly not compared to cars. As

0:18:26.240 --> 0:18:28.400
<v Speaker 1>it turns out there are more cars and there are

0:18:28.520 --> 0:18:33.879
<v Speaker 1>volcanoes or factory power facilities. Yeah. Um, And so there

0:18:33.880 --> 0:18:36.600
<v Speaker 1>are a few questions. Okay, so we're we're seeing this

0:18:36.720 --> 0:18:40.960
<v Speaker 1>correlation between temperature and the concentration of CO two in

0:18:41.000 --> 0:18:44.000
<v Speaker 1>the atmosphere. Um, but are there other things that might

0:18:44.040 --> 0:18:46.600
<v Speaker 1>be causing it instead. Well, we don't know for sure,

0:18:46.640 --> 0:18:50.920
<v Speaker 1>but most scientists think not. Um. Well, you know, I mean,

0:18:51.119 --> 0:18:53.600
<v Speaker 1>you know, alterations in them in the Earth's orbit and

0:18:53.680 --> 0:18:56.960
<v Speaker 1>the Sun's orbit can change change the climate over a

0:18:56.960 --> 0:18:59.760
<v Speaker 1>given period of time, but not the drastic way that

0:18:59.800 --> 0:19:02.320
<v Speaker 1>we seen it in the past couple decades. Yeah. Like

0:19:02.400 --> 0:19:07.080
<v Speaker 1>some objections you might see sometimes people who say like, oh,

0:19:07.119 --> 0:19:09.960
<v Speaker 1>the Sun is just hotter, like it's warming the Earth

0:19:10.040 --> 0:19:13.760
<v Speaker 1>more than before. But we can actually test that hypothesis

0:19:13.800 --> 0:19:16.880
<v Speaker 1>and that doesn't really stand up apparently, right, the Sun's

0:19:16.960 --> 0:19:19.880
<v Speaker 1>energy varies on about an eleven year cycle. Um, it

0:19:20.000 --> 0:19:22.679
<v Speaker 1>might vary also on a on a greater cycle, but

0:19:22.760 --> 0:19:25.960
<v Speaker 1>we haven't had enough data yet to tell whether that's true.

0:19:26.080 --> 0:19:30.960
<v Speaker 1>And um, as of early the solar brightness since two

0:19:30.960 --> 0:19:34.239
<v Speaker 1>thousand five has actually been slightly lower yeah than in

0:19:34.280 --> 0:19:37.520
<v Speaker 1>the past, So yet we have a warming trend during

0:19:37.560 --> 0:19:40.640
<v Speaker 1>that time. The bottom line is, uh, we're pretty sure

0:19:40.720 --> 0:19:43.840
<v Speaker 1>that there is a substantial link between the amount of

0:19:43.880 --> 0:19:47.480
<v Speaker 1>C O two especially, but other greenhouse gases like methane,

0:19:47.640 --> 0:19:52.520
<v Speaker 1>chlor flora carbons and stuff like that, and the greenhouse

0:19:52.560 --> 0:19:55.880
<v Speaker 1>effect that is causing the global warming trend we see, right,

0:19:55.960 --> 0:19:58.120
<v Speaker 1>So let's um, I guess then we need to talk

0:19:58.119 --> 0:20:00.119
<v Speaker 1>about some of the effects here, and we've touched on

0:20:00.240 --> 0:20:03.240
<v Speaker 1>these obviously, because if you're talking about global warming, a

0:20:03.280 --> 0:20:06.720
<v Speaker 1>lot of effects become fairly self evident, but some of

0:20:06.720 --> 0:20:09.400
<v Speaker 1>them you might not realize at first because they're kind

0:20:09.400 --> 0:20:12.400
<v Speaker 1>of a it's kind of like a domino effect. Right, So,

0:20:12.520 --> 0:20:14.800
<v Speaker 1>what's global warming going to do in the future? All right? Well,

0:20:14.840 --> 0:20:21.840
<v Speaker 1>first of all, I sounded so, yeah, here's a trend

0:20:21.960 --> 0:20:24.399
<v Speaker 1>that we're observing. What's it really going to do in

0:20:24.440 --> 0:20:28.440
<v Speaker 1>the future? Okay, Well, um, there's there are a lot

0:20:28.480 --> 0:20:31.440
<v Speaker 1>of a lot of disagreements, well, maybe not disagreements. There's

0:20:31.480 --> 0:20:35.880
<v Speaker 1>a lot of debate and conversation around this because frankly,

0:20:35.920 --> 0:20:38.960
<v Speaker 1>climate is an incredibly complex thing. There are a lot

0:20:39.000 --> 0:20:42.160
<v Speaker 1>of different factors that all influence one another in different ways,

0:20:42.520 --> 0:20:47.240
<v Speaker 1>and changing the temperature of the Earth is definitely changing climates.

0:20:47.520 --> 0:20:50.480
<v Speaker 1>It's just a question of how drastically are certain climates

0:20:50.480 --> 0:20:52.520
<v Speaker 1>going to change. And you know, once you get to

0:20:52.560 --> 0:20:54.560
<v Speaker 1>a point where you're trying to predict what's happening in

0:20:54.560 --> 0:20:58.320
<v Speaker 1>a particular region, it really gets tricky, right, right, So,

0:20:58.359 --> 0:21:01.240
<v Speaker 1>in other words, saying this is exactly how it's going

0:21:01.280 --> 0:21:05.560
<v Speaker 1>to affect the northeastern United States would be probably an

0:21:05.600 --> 0:21:09.800
<v Speaker 1>irresponsible thing to say as a scientist, unless you were

0:21:09.840 --> 0:21:13.880
<v Speaker 1>able to couch that in probabilities, making probabilistic models, where

0:21:13.920 --> 0:21:16.640
<v Speaker 1>you say there's a certain percentage of likelihood that this

0:21:16.760 --> 0:21:19.240
<v Speaker 1>is going to happen. But keep in mind that's a

0:21:19.280 --> 0:21:22.119
<v Speaker 1>percentage of likelihood, right, and there are just too many,

0:21:22.160 --> 0:21:25.119
<v Speaker 1>too many factors, too many points of data to really

0:21:25.240 --> 0:21:27.919
<v Speaker 1>be certain about that kind of thing. Yeah, and anytime

0:21:28.000 --> 0:21:31.320
<v Speaker 1>we're dealing in um future projections, instead of just say

0:21:31.400 --> 0:21:34.520
<v Speaker 1>I don't know, basic empirical observations. We're talking in terms

0:21:34.520 --> 0:21:38.320
<v Speaker 1>of likelihood certainty. Seeing even with these things that were

0:21:38.480 --> 0:21:42.800
<v Speaker 1>very sure about if it's future speculation, it's like, we're

0:21:44.119 --> 0:21:48.520
<v Speaker 1>not actually positive. And in fact, there there are percentages

0:21:48.560 --> 0:21:52.800
<v Speaker 1>that are like that, there's essentially certainty that we're going

0:21:52.840 --> 0:21:57.359
<v Speaker 1>to see uh increased heat waves in the future. So

0:21:57.680 --> 0:22:02.800
<v Speaker 1>that's scientists have put that uh a near certainty. Other

0:22:02.840 --> 0:22:06.760
<v Speaker 1>ones are you know, at different ranges. But for instance, ice,

0:22:07.320 --> 0:22:11.080
<v Speaker 1>we can we're gonna see less of it. Yeah, there's

0:22:11.080 --> 0:22:13.200
<v Speaker 1>gonna be a lot of melting. So we're gonna see

0:22:13.200 --> 0:22:15.080
<v Speaker 1>a loss of sea ice. We're gonna see reduction in

0:22:15.080 --> 0:22:19.400
<v Speaker 1>glacier sizes. We're gonna see ice breaking up and melting

0:22:19.480 --> 0:22:22.440
<v Speaker 1>earlier in the year on lakes and rivers and places

0:22:22.440 --> 0:22:25.200
<v Speaker 1>where it does freeze over right. That's because every year

0:22:25.400 --> 0:22:28.359
<v Speaker 1>um ice will will reform in the winter and then

0:22:28.400 --> 0:22:30.600
<v Speaker 1>melting down in the summer. And when they talk about

0:22:30.640 --> 0:22:33.359
<v Speaker 1>the glaciers melting, it's not that they're all doing it

0:22:33.400 --> 0:22:36.359
<v Speaker 1>all at once. Forever's um it's it's just that less

0:22:36.440 --> 0:22:39.720
<v Speaker 1>ice is being recaptured in the winter than it was

0:22:39.760 --> 0:22:42.880
<v Speaker 1>the previous So the overall trend is that the glaciers

0:22:42.880 --> 0:22:46.200
<v Speaker 1>are getting smaller in size and over time. And then

0:22:46.359 --> 0:22:50.600
<v Speaker 1>you also we see decrease decreases in snow packs, which

0:22:50.640 --> 0:22:53.439
<v Speaker 1>means you're going to see some actual ecosystems change as

0:22:53.440 --> 0:22:55.560
<v Speaker 1>a result. And by the way, all of this ice

0:22:55.680 --> 0:23:00.000
<v Speaker 1>melting and decreases in snow winds up creating warmer temper

0:23:00.080 --> 0:23:03.680
<v Speaker 1>cheers overall, because ice and snow are reflective, whereas um

0:23:03.880 --> 0:23:06.919
<v Speaker 1>warm ground or warm water or even I mean, you know,

0:23:07.000 --> 0:23:11.040
<v Speaker 1>room temperature ground or water are darker and therefore absorb

0:23:11.119 --> 0:23:14.119
<v Speaker 1>more of that heat coming down from the sun. Ye uh.

0:23:14.320 --> 0:23:17.560
<v Speaker 1>NASA says that the green Land and Antarctic ice sheets

0:23:17.560 --> 0:23:21.159
<v Speaker 1>have decreased in mass UH from two thousand two to

0:23:21.200 --> 0:23:24.200
<v Speaker 1>two thousand and six. They estimate that Greenland lost between

0:23:24.240 --> 0:23:28.119
<v Speaker 1>a hundred fifty cubic kilometers or thirty six to sixty

0:23:28.160 --> 0:23:31.800
<v Speaker 1>cubic miles of ice per year, and an Arcticle lost

0:23:31.800 --> 0:23:34.680
<v Speaker 1>about a hundred fifty two cubic kilometers or thirty six

0:23:34.720 --> 0:23:37.000
<v Speaker 1>cubic miles of ice between two thousand two and two

0:23:37.000 --> 0:23:39.800
<v Speaker 1>thousand five. So an Arctica is not losing it at

0:23:39.840 --> 0:23:43.520
<v Speaker 1>the same rate as Greenland, but it's still losing ice

0:23:44.400 --> 0:23:47.639
<v Speaker 1>on top of that we're seeing the possibility of of

0:23:48.280 --> 0:23:53.040
<v Speaker 1>drastically shifting weather patterns. We're talking massive changes in precipitation levels,

0:23:53.040 --> 0:23:56.600
<v Speaker 1>so the day after tomorrow, not that dramatic in that

0:23:57.440 --> 0:24:00.679
<v Speaker 1>quick Not not this this flip flopping effect where you

0:24:00.720 --> 0:24:04.720
<v Speaker 1>suddenly have temperatures dropped to thirty below zero in a

0:24:04.720 --> 0:24:07.119
<v Speaker 1>blink of an eye, but rather that you're going to

0:24:07.160 --> 0:24:10.520
<v Speaker 1>see areas get more rain than they normally would, while

0:24:10.600 --> 0:24:13.840
<v Speaker 1>other areas become get less rain and end up having

0:24:14.119 --> 0:24:18.959
<v Speaker 1>severe droughts. Um but not intelligent droughts, not not as

0:24:19.000 --> 0:24:21.480
<v Speaker 1>far as I can determine. They might still chase Jake

0:24:21.560 --> 0:24:23.879
<v Speaker 1>Jillen Hall, because wouldn't we all? I would like to

0:24:23.920 --> 0:24:27.439
<v Speaker 1>have an intelligent drought on this podcast to replace a

0:24:27.440 --> 0:24:30.879
<v Speaker 1>certain co host who's getting a little, little, little little

0:24:30.880 --> 0:24:33.960
<v Speaker 1>beans in the system. I'm just kidding too. He can

0:24:34.000 --> 0:24:37.800
<v Speaker 1>sit next to you. So yeah, we're changes in precipitation levels. Also,

0:24:37.960 --> 0:24:41.880
<v Speaker 1>projections suggest that there's a possibility that will see more

0:24:41.960 --> 0:24:46.240
<v Speaker 1>rainfall in high latitudes and less rainfall in subtropical climates.

0:24:46.320 --> 0:24:50.240
<v Speaker 1>So that's going to dramatically change those ecosystems, which brings

0:24:50.280 --> 0:24:53.520
<v Speaker 1>me to other ecosystem changes, plant and animal ranges are

0:24:53.560 --> 0:24:56.560
<v Speaker 1>going to shift as environments become less suitable for over time.

0:24:56.600 --> 0:24:59.639
<v Speaker 1>We've already started to see that where we're seeing animal

0:24:59.680 --> 0:25:03.600
<v Speaker 1>popular lations move from where they traditionally would range because

0:25:03.840 --> 0:25:06.639
<v Speaker 1>those areas are no longer suitable for them. That's going

0:25:06.680 --> 0:25:10.399
<v Speaker 1>to continue. In Latin America, UH rainforests are starting to

0:25:10.520 --> 0:25:14.040
<v Speaker 1>change over into savannah's now. That means that there's also

0:25:14.200 --> 0:25:18.920
<v Speaker 1>been a decrease in precipitation there, which means that there's

0:25:19.119 --> 0:25:23.440
<v Speaker 1>uh greater strain on fresh water resources, so people are

0:25:23.440 --> 0:25:26.280
<v Speaker 1>having to work harder to get fresh water in those areas.

0:25:26.680 --> 0:25:29.320
<v Speaker 1>Also means that because the rainforest is converting over to

0:25:29.359 --> 0:25:32.680
<v Speaker 1>a different kind of ecosystem, you're seeing a real risk

0:25:32.840 --> 0:25:35.639
<v Speaker 1>to bio diversity. Lots of species that are put at

0:25:35.720 --> 0:25:40.080
<v Speaker 1>risk because of that loss of their environment. In Europe,

0:25:40.119 --> 0:25:43.160
<v Speaker 1>there's been an increase in flash floods and coastal flooding.

0:25:43.400 --> 0:25:46.720
<v Speaker 1>Projections for Africa indicate that severe droughts and larger strain

0:25:46.760 --> 0:25:48.840
<v Speaker 1>of water resources will be in the near future. That

0:25:48.880 --> 0:25:52.000
<v Speaker 1>of course, will also affect food resources. We've discussed this

0:25:52.040 --> 0:25:54.120
<v Speaker 1>in the past, how water and food are so closely related.

0:25:55.000 --> 0:25:57.960
<v Speaker 1>Asia is also going to experience increased flooding and decreased

0:25:57.960 --> 0:26:01.200
<v Speaker 1>access to fresh water, so lots of rough things. They're

0:26:01.520 --> 0:26:05.000
<v Speaker 1>on top of that, the ocean is being affected in

0:26:05.200 --> 0:26:08.080
<v Speaker 1>a couple of different ways. A salinity is changing, that's

0:26:08.359 --> 0:26:12.640
<v Speaker 1>the amount of salt concentration in the oceans um that changes,

0:26:12.760 --> 0:26:16.400
<v Speaker 1>and drawing on observations from nineteen fifty five to two

0:26:16.440 --> 0:26:20.840
<v Speaker 1>thousand four, researchers found that the ocean sealinity changed throughout

0:26:21.080 --> 0:26:23.560
<v Speaker 1>the study period, and that the changes were independent of

0:26:23.680 --> 0:26:27.479
<v Speaker 1>known natural variability, and that the shifts were consistent with

0:26:27.600 --> 0:26:31.800
<v Speaker 1>the expected effects of anthropogenic climate change. So, in other words,

0:26:32.200 --> 0:26:36.040
<v Speaker 1>this is not due to some sort of undersea activity

0:26:36.160 --> 0:26:41.920
<v Speaker 1>or natural cycle. This is something means caused by by humankind.

0:26:42.760 --> 0:26:45.960
<v Speaker 1>The pH of oceans is changing. This is because when

0:26:46.000 --> 0:26:50.680
<v Speaker 1>carbon dioxide reacts with seawater, it lowers the pH of

0:26:50.720 --> 0:26:53.240
<v Speaker 1>the sea water. Uh so that means it makes it

0:26:53.320 --> 0:26:57.399
<v Speaker 1>more acidic um, which if you've ever had a a

0:26:57.400 --> 0:26:59.880
<v Speaker 1>fish tank at home, and that could be a bad thing.

0:27:00.040 --> 0:27:03.760
<v Speaker 1>That thing. Yeah, so it absorbs a lot of carbon

0:27:03.840 --> 0:27:06.800
<v Speaker 1>dioxide and it that kind of does that, you know,

0:27:06.840 --> 0:27:09.399
<v Speaker 1>it just does that naturally over over a long period

0:27:09.440 --> 0:27:12.240
<v Speaker 1>of time. It would absorb like if we were to

0:27:12.320 --> 0:27:16.399
<v Speaker 1>stop producing CO two today and and only natural sources

0:27:16.440 --> 0:27:19.320
<v Speaker 1>were producing it. Uh, the ocean would end up absorbing

0:27:19.520 --> 0:27:22.080
<v Speaker 1>that CEO two over the course of you know, a

0:27:22.119 --> 0:27:26.920
<v Speaker 1>couple of thousand years. Um. But uh, it's and that

0:27:26.960 --> 0:27:30.120
<v Speaker 1>would dramatically change that ocean over that time. But we're

0:27:30.119 --> 0:27:32.359
<v Speaker 1>also talking about using the ocean as a possible sink

0:27:32.600 --> 0:27:36.720
<v Speaker 1>for carbon dioxide, which we'll talk more about in another podcast.

0:27:36.720 --> 0:27:40.800
<v Speaker 1>But that would mean pumping up the acidity level of

0:27:40.840 --> 0:27:43.159
<v Speaker 1>the oceans, at least in a regional area wherever the

0:27:43.160 --> 0:27:46.320
<v Speaker 1>pumping was being done. Uh, in a in a time

0:27:46.320 --> 0:27:49.080
<v Speaker 1>scale that would be much shorter than what we would

0:27:49.119 --> 0:27:51.879
<v Speaker 1>see naturally. So in other words, we'd be seeing something

0:27:51.920 --> 0:27:54.200
<v Speaker 1>happening in the oceans that is akin to what we're

0:27:54.200 --> 0:27:57.000
<v Speaker 1>seeing in our atmosphere right now. It would be the

0:27:57.000 --> 0:27:59.360
<v Speaker 1>the effects would be different, but it's the same sort

0:27:59.359 --> 0:28:03.040
<v Speaker 1>of thing where you know, it's not necessarily a solution

0:28:03.080 --> 0:28:05.520
<v Speaker 1>to a problem, it's creating a different problem. It's it's

0:28:05.560 --> 0:28:07.720
<v Speaker 1>it's sort of a lateral shift. On top of that,

0:28:07.760 --> 0:28:11.320
<v Speaker 1>we're talking about the complexity of climate. You know, It's

0:28:11.359 --> 0:28:13.960
<v Speaker 1>like we said, it's it's complicated stuff. There's so many

0:28:13.960 --> 0:28:16.960
<v Speaker 1>different things to bring into consideration that it is very

0:28:17.000 --> 0:28:20.160
<v Speaker 1>difficult for us to say for sure what is going

0:28:20.200 --> 0:28:23.600
<v Speaker 1>to happen in the future. It's just, uh, we know

0:28:23.680 --> 0:28:26.840
<v Speaker 1>that these basic things are very likely to happen. When

0:28:26.840 --> 0:28:29.920
<v Speaker 1>you get more specific, like, well we see greater cyclone

0:28:29.960 --> 0:28:33.440
<v Speaker 1>activity and intensity in the future, that's a possibility, but

0:28:33.680 --> 0:28:36.400
<v Speaker 1>it's not a certainty. And I think that's r rated

0:28:36.520 --> 0:28:39.360
<v Speaker 1>about the sixty six percent level of certainty, which is

0:28:39.400 --> 0:28:44.840
<v Speaker 1>still over more certain than not, but still a pretty

0:28:44.880 --> 0:28:47.600
<v Speaker 1>huge But then when it comes to things like you know,

0:28:47.640 --> 0:28:50.040
<v Speaker 1>there'll be more heat waves and there will be less

0:28:50.080 --> 0:28:52.160
<v Speaker 1>rain in some areas and more rain in other areas,

0:28:52.160 --> 0:28:57.000
<v Speaker 1>the certainty level is way higher like or above. So

0:28:57.000 --> 0:28:59.280
<v Speaker 1>so there are some things that we just cannot know

0:28:59.520 --> 0:29:01.840
<v Speaker 1>right now because we don't have all the information we

0:29:01.880 --> 0:29:05.640
<v Speaker 1>would need to project an accurate model. And it's just

0:29:05.720 --> 0:29:09.160
<v Speaker 1>so hard to project in this realm because you're not

0:29:09.200 --> 0:29:13.520
<v Speaker 1>talking about, say, predicting a chemical reaction and a beaker

0:29:13.600 --> 0:29:18.440
<v Speaker 1>that's isolated. The climate is something that creates feedback loops

0:29:18.480 --> 0:29:22.480
<v Speaker 1>within itself, so lots of different climate variables influence the

0:29:22.520 --> 0:29:27.280
<v Speaker 1>other ones. Uh, it influences whether weather influences ecosystems which

0:29:27.280 --> 0:29:31.000
<v Speaker 1>affect the climate, and so there's just it's it's incredibly

0:29:31.320 --> 0:29:34.240
<v Speaker 1>complex system and only that, but we can't even be

0:29:34.320 --> 0:29:38.920
<v Speaker 1>certain how much greenhouse gas we're emitting on any given day,

0:29:39.240 --> 0:29:42.360
<v Speaker 1>let alone. Like we can make estimates, but those estimates

0:29:42.360 --> 0:29:45.440
<v Speaker 1>are based upon information that researchers can gather. And when

0:29:45.480 --> 0:29:48.480
<v Speaker 1>you think about it, that the world's a big place. Yeah,

0:29:48.600 --> 0:29:51.840
<v Speaker 1>the UM So, like the estimates I was using earlier,

0:29:51.880 --> 0:29:56.080
<v Speaker 1>they come from the Manoloa Observatory in Hawaii, and that

0:29:56.080 --> 0:30:00.400
<v Speaker 1>that consistently has been collecting uh data on the atmospheric

0:30:00.520 --> 0:30:03.560
<v Speaker 1>concentration of carbon dioxide for a while now, and so

0:30:03.640 --> 0:30:07.040
<v Speaker 1>that can pretty steadily track what's going on. But the

0:30:07.120 --> 0:30:10.760
<v Speaker 1>concentration might not be UM. Actually don't know the answer

0:30:10.760 --> 0:30:14.760
<v Speaker 1>to this, whether it's concentrated more in some places than others,

0:30:14.840 --> 0:30:17.720
<v Speaker 1>or if it's pretty well dispersed. Yeah. Well, I mean

0:30:17.800 --> 0:30:20.840
<v Speaker 1>the point being that even you know, even if if

0:30:20.920 --> 0:30:24.800
<v Speaker 1>one nation were to cut out all carbon emissions, unless

0:30:24.920 --> 0:30:28.200
<v Speaker 1>every other nation did so as well, Uh, you know,

0:30:28.600 --> 0:30:31.480
<v Speaker 1>the the effect might be small at least in the

0:30:31.520 --> 0:30:33.880
<v Speaker 1>short term. Maybe in the long term it would make

0:30:34.040 --> 0:30:35.880
<v Speaker 1>a pretty big difference, But in the short term it

0:30:35.920 --> 0:30:38.920
<v Speaker 1>would be negligible. We would have to have a much

0:30:39.080 --> 0:30:44.000
<v Speaker 1>larger effort to really make a huge impact. Okay, So

0:30:44.280 --> 0:30:49.400
<v Speaker 1>looking forward into the future, we are certain that the

0:30:49.440 --> 0:30:52.080
<v Speaker 1>Earth is warming, and the trend is that it's going

0:30:52.160 --> 0:30:57.920
<v Speaker 1>to continue warming. We're very confident that human activity has

0:30:57.960 --> 0:31:02.720
<v Speaker 1>caused this, and there are predictions we've made about lots

0:31:02.760 --> 0:31:06.880
<v Speaker 1>of possibly very negative consequences of this, with varying degrees

0:31:06.880 --> 0:31:11.000
<v Speaker 1>of certainty with each of those predictions. Um, what what

0:31:11.040 --> 0:31:15.520
<v Speaker 1>do we do next? Well? First, uh, I mean a

0:31:15.600 --> 0:31:17.640
<v Speaker 1>lot of that we're going to address in our next episode.

0:31:17.640 --> 0:31:20.160
<v Speaker 1>But first I think we need to talk a little

0:31:20.160 --> 0:31:23.880
<v Speaker 1>bit about the concept of a scientific consensus. Yeah, there's

0:31:23.880 --> 0:31:26.920
<v Speaker 1>sort of a public conversation going on about global warming.

0:31:26.960 --> 0:31:29.840
<v Speaker 1>In case you haven't noticed change you're not on Twitter

0:31:29.960 --> 0:31:33.160
<v Speaker 1>or something. Uh, So the scientific consensus is one of

0:31:33.200 --> 0:31:37.640
<v Speaker 1>those terms that I think, uh, gets thrown around a lot,

0:31:37.720 --> 0:31:41.920
<v Speaker 1>and there's not a full understanding and in the general

0:31:41.920 --> 0:31:45.120
<v Speaker 1>public about what that means. Yeah. Okay, Well let's just

0:31:45.520 --> 0:31:48.760
<v Speaker 1>do a little experiment here. Imagine I am a lay person,

0:31:49.560 --> 0:31:53.000
<v Speaker 1>uh that doesn't have a lot of expertise on climate science.

0:31:53.040 --> 0:31:57.400
<v Speaker 1>That's not hard to imagine. Um, But go on, but

0:31:57.480 --> 0:32:02.560
<v Speaker 1>I recognize that there's this public to eight about climate change,

0:32:02.560 --> 0:32:06.080
<v Speaker 1>and specifically, I think the most contentious part of the

0:32:06.120 --> 0:32:11.760
<v Speaker 1>debate is the anthropogenic part, whether humans are causing this um,

0:32:11.800 --> 0:32:14.360
<v Speaker 1>which I guess affects the idea of whether or not

0:32:14.480 --> 0:32:16.800
<v Speaker 1>we can we have the power to stop it, or

0:32:16.840 --> 0:32:19.720
<v Speaker 1>if we should, if we should take any efforts to

0:32:19.760 --> 0:32:22.400
<v Speaker 1>stop it because of the potential impact that would have

0:32:22.600 --> 0:32:27.040
<v Speaker 1>on economy, lifestyle side. Um. So, I am a lay person.

0:32:27.120 --> 0:32:29.840
<v Speaker 1>I have no expertise in this area, and I noticed

0:32:29.880 --> 0:32:32.680
<v Speaker 1>that there are people who both seem to know more

0:32:32.720 --> 0:32:35.840
<v Speaker 1>than me about it arguing about it. So how do

0:32:35.880 --> 0:32:38.560
<v Speaker 1>I make a decision? How do I form an opinion

0:32:38.600 --> 0:32:42.080
<v Speaker 1>about this that's over my head? Well, the scientific consensus

0:32:42.080 --> 0:32:44.000
<v Speaker 1>in this case, when we talk about consensus, you're talking

0:32:44.040 --> 0:32:47.200
<v Speaker 1>about a a large group of people who have all

0:32:47.720 --> 0:32:52.360
<v Speaker 1>uh kind of come to the same conclusions, uh perhaps independently,

0:32:52.880 --> 0:32:58.440
<v Speaker 1>and they are presenting a united front at least on

0:32:58.520 --> 0:33:03.560
<v Speaker 1>some level on the issue. Well, what is the consensus? What? Like?

0:33:03.640 --> 0:33:07.280
<v Speaker 1>How many people agree about this? In In a study

0:33:07.320 --> 0:33:12.400
<v Speaker 1>of papers that were expressing a position on um anthropogenic

0:33:12.480 --> 0:33:17.840
<v Speaker 1>global warming, point one percent endorsed the consensus that humans

0:33:17.920 --> 0:33:21.400
<v Speaker 1>are in fact causing it. Yeah, that's a that's a

0:33:21.480 --> 0:33:26.120
<v Speaker 1>huge scientific consensus there. This is from a literature review

0:33:26.160 --> 0:33:30.720
<v Speaker 1>that was published in called Quantifying the Consensus on Intropogenic

0:33:30.760 --> 0:33:33.240
<v Speaker 1>Global Warming in the Scientific Literature, that the one in

0:33:33.440 --> 0:33:38.120
<v Speaker 1>Environmental Research letters. That is indeed. Um. So, the way

0:33:38.160 --> 0:33:42.080
<v Speaker 1>this the study progressed, as I understand it is they

0:33:42.120 --> 0:33:44.960
<v Speaker 1>looked at all these different reports and they looked for

0:33:45.040 --> 0:33:51.640
<v Speaker 1>any mention of the causation for whatever the warming or

0:33:51.680 --> 0:33:56.560
<v Speaker 1>climate change effect was, right, reports in fact and so

0:33:58.440 --> 0:34:01.320
<v Speaker 1>eleven correct. Well, let's us read from the abstract to

0:34:01.880 --> 0:34:04.600
<v Speaker 1>have some clarity here. Sure, they say, we analyze the

0:34:04.640 --> 0:34:07.960
<v Speaker 1>evolution of the scientific consensus on anthropogenic global warming and

0:34:08.000 --> 0:34:12.160
<v Speaker 1>the peer reviewed scientific literature. Examining eleven forty four climate

0:34:12.200 --> 0:34:17.240
<v Speaker 1>abstracts from two eleven matching the topics global climate change

0:34:17.360 --> 0:34:20.719
<v Speaker 1>or global warming, we find that sixty six point four

0:34:20.760 --> 0:34:26.440
<v Speaker 1>percent of abstracts expressed no position on a GW, thirty

0:34:26.440 --> 0:34:30.160
<v Speaker 1>two point six percent endorsed it, points seven percent rejected it,

0:34:30.239 --> 0:34:33.120
<v Speaker 1>and point three percent were uncertain about it. So, in

0:34:33.160 --> 0:34:35.719
<v Speaker 1>other words, out of the ones that actually addressed what

0:34:35.880 --> 0:34:40.360
<v Speaker 1>the cause was, point one percent said it was anthropogenic.

0:34:40.880 --> 0:34:45.000
<v Speaker 1>And then the but I understand that some people are

0:34:45.000 --> 0:34:47.640
<v Speaker 1>framing this in a different way. Well, yeah, actually this

0:34:47.719 --> 0:34:50.719
<v Speaker 1>is a good example of how, um, sometimes it can

0:34:50.760 --> 0:34:53.920
<v Speaker 1>be difficult to interpret scientific literature. I was just looking

0:34:53.920 --> 0:34:56.080
<v Speaker 1>around about this paper. I found one blog post on

0:34:56.120 --> 0:34:58.960
<v Speaker 1>the internet that was like, look, you know, out of

0:34:58.960 --> 0:35:02.080
<v Speaker 1>all these scientists, so thirty two point six percent endorsed it,

0:35:02.200 --> 0:35:06.319
<v Speaker 1>So that's the minority. Um, ignoring the fact that, Yeah,

0:35:06.600 --> 0:35:11.200
<v Speaker 1>so sixty percent of the papers examined in this study

0:35:11.640 --> 0:35:16.040
<v Speaker 1>didn't express an opinion. They didn't address about what caused it,

0:35:16.160 --> 0:35:19.799
<v Speaker 1>whether it was anthropogenic or not. Um, they were you know,

0:35:19.840 --> 0:35:23.479
<v Speaker 1>they just didn't address that issue. But so they looked

0:35:23.480 --> 0:35:25.960
<v Speaker 1>at that and said like, oh, look it's it's the

0:35:26.000 --> 0:35:29.520
<v Speaker 1>minority now. Um, of course it's not the minority in fact.

0:35:30.160 --> 0:35:33.200
<v Speaker 1>On between, Yeah, as we've just been pointing out of

0:35:33.320 --> 0:35:35.960
<v Speaker 1>the papers that did express an opinion whether it was

0:35:36.120 --> 0:35:40.720
<v Speaker 1>caused by humans or not, said that it was right.

0:35:40.840 --> 0:35:44.040
<v Speaker 1>So that is a pretty that's a pretty uh big

0:35:44.080 --> 0:35:47.759
<v Speaker 1>consensus there. Yeah, and only that, But beyond that, there

0:35:47.800 --> 0:35:54.719
<v Speaker 1>have been plenty of of climatologist gatherings where more and

0:35:54.760 --> 0:35:57.520
<v Speaker 1>more people are just saying like, no, that the scientific

0:35:57.520 --> 0:36:01.560
<v Speaker 1>community at at large says that this is something that's happening.

0:36:01.800 --> 0:36:04.080
<v Speaker 1>That doesn't mean that there aren't people who disagree, but

0:36:04.200 --> 0:36:08.400
<v Speaker 1>they are in a very tiny sliver, right. And we

0:36:08.440 --> 0:36:11.080
<v Speaker 1>do want to say that we absolutely support skepticism. I

0:36:11.080 --> 0:36:13.640
<v Speaker 1>think all three of us are are pretty big skeptics

0:36:13.680 --> 0:36:17.760
<v Speaker 1>in general. We really appreciate the rigor of scientific research.

0:36:17.800 --> 0:36:20.240
<v Speaker 1>You know, we want questions to be asked. That questions

0:36:20.280 --> 0:36:24.000
<v Speaker 1>being asked is the entire point of science. But if

0:36:24.040 --> 0:36:29.319
<v Speaker 1>you aren't asking questions, if you're simply dissenting, then if

0:36:29.320 --> 0:36:33.759
<v Speaker 1>you're simply denying something, then you're not really being scientific.

0:36:33.800 --> 0:36:36.719
<v Speaker 1>And you know so. In other words, what I would

0:36:36.719 --> 0:36:40.279
<v Speaker 1>tell the lay person is that the majority of scientists

0:36:40.400 --> 0:36:44.319
<v Speaker 1>who have devoted their their professional lives to studying this

0:36:45.080 --> 0:36:49.360
<v Speaker 1>say that one, it's a thing, to it's it's being caused,

0:36:49.400 --> 0:36:52.960
<v Speaker 1>at least in part by human activity, and that therefore

0:36:53.040 --> 0:36:57.279
<v Speaker 1>we could do something that would reduce that um that

0:36:57.400 --> 0:37:02.279
<v Speaker 1>those far outnumber the dissenting of and that it's not

0:37:02.920 --> 0:37:05.719
<v Speaker 1>to say the scientists is smarter than you are, but

0:37:05.840 --> 0:37:08.720
<v Speaker 1>rather that here's all the research that they have done

0:37:09.360 --> 0:37:13.839
<v Speaker 1>that has been reviewed and replicated. Well, it's not just

0:37:13.960 --> 0:37:17.080
<v Speaker 1>that scientists are smart in fact, it's not even just

0:37:17.239 --> 0:37:19.799
<v Speaker 1>that scientists are the people who spend a lot of

0:37:19.800 --> 0:37:22.440
<v Speaker 1>time studying this, though both of those things tend to

0:37:22.480 --> 0:37:25.719
<v Speaker 1>be true. Um, it's you're trusted when you trust in

0:37:25.760 --> 0:37:28.760
<v Speaker 1>the scientific consensus. You trust not just in a person,

0:37:28.840 --> 0:37:32.240
<v Speaker 1>but in a process. You're you're trusting in the fact

0:37:32.400 --> 0:37:36.160
<v Speaker 1>that the way, um, the scientific community works is that

0:37:36.640 --> 0:37:40.200
<v Speaker 1>everybody's trying to prove each other wrong. Right, there's huge

0:37:40.200 --> 0:37:43.640
<v Speaker 1>rewards for proving someone wrong with math. The way you

0:37:43.680 --> 0:37:48.799
<v Speaker 1>would get accolades and attract a lot of uh, you

0:37:48.800 --> 0:37:55.120
<v Speaker 1>know money, essentially is to um, look to say, actually,

0:37:55.200 --> 0:37:57.600
<v Speaker 1>everybody's wrong about this, and here's why. And if you

0:37:57.800 --> 0:38:01.239
<v Speaker 1>produce a good argument, people look at and they say,

0:38:01.239 --> 0:38:03.520
<v Speaker 1>oh wait a minute, yeah, we do need to review

0:38:04.320 --> 0:38:07.920
<v Speaker 1>our our opinions. Um, that's how you become famous as

0:38:07.920 --> 0:38:10.279
<v Speaker 1>a scientist. Well, it's also think about most of the

0:38:10.320 --> 0:38:15.760
<v Speaker 1>most famous scientists are people who changed opinions in their field. Sure, sure,

0:38:15.800 --> 0:38:19.319
<v Speaker 1>and it's but I mean, the the thing we're looking

0:38:19.360 --> 0:38:22.040
<v Speaker 1>at here, and I mean I completely agree, but the

0:38:22.080 --> 0:38:26.120
<v Speaker 1>thing is for the scientific consensus here is that I

0:38:26.200 --> 0:38:28.000
<v Speaker 1>want to make sure that our listeners know we're not

0:38:28.360 --> 0:38:33.240
<v Speaker 1>advocating you fall into the rhetorical fallacy of argument from authority,

0:38:33.320 --> 0:38:36.200
<v Speaker 1>which is one of those ideas where you say, because

0:38:36.239 --> 0:38:38.560
<v Speaker 1>this person is an authority in this place, everything they

0:38:38.600 --> 0:38:41.680
<v Speaker 1>say is right. But we're really saying is that there's

0:38:41.719 --> 0:38:44.239
<v Speaker 1>been a massive amount of research. It all points to

0:38:44.280 --> 0:38:47.960
<v Speaker 1>the same way. The scientific community at large agrees upon it.

0:38:48.800 --> 0:38:52.120
<v Speaker 1>We're giving authority to their to their numbers and their methodology,

0:38:52.360 --> 0:38:56.000
<v Speaker 1>not them themselves exactly well, And the fact that even

0:38:56.040 --> 0:38:59.640
<v Speaker 1>this consensus doesn't mean that it's right. It just gives

0:38:59.680 --> 0:39:04.480
<v Speaker 1>you a more greater confidence that's right. Because in any case,

0:39:05.239 --> 0:39:08.359
<v Speaker 1>if you don't know exactly for yourself, and nobody really

0:39:08.360 --> 0:39:11.680
<v Speaker 1>does on these issues, you are making a value judgment.

0:39:11.880 --> 0:39:16.680
<v Speaker 1>You know, you're sure you're estimating probability. Right. As more

0:39:16.840 --> 0:39:19.239
<v Speaker 1>people who know a whole lot about this kind of

0:39:19.280 --> 0:39:25.320
<v Speaker 1>thing agree, the probability that they're wrong is probably is decreasing, right, exactly,

0:39:25.360 --> 0:39:28.960
<v Speaker 1>So could a lone voice of descent be correct and

0:39:29.080 --> 0:39:32.360
<v Speaker 1>say that all of these studies are wrong and in

0:39:32.480 --> 0:39:37.279
<v Speaker 1>fact they were all misinterpreted. But that but that possibility

0:39:37.640 --> 0:39:41.440
<v Speaker 1>is smaller, incredibly tiny, I mean very very tiny. Doesn't

0:39:41.480 --> 0:39:45.160
<v Speaker 1>mean that it's impossible. It just means it's not plausible. Um,

0:39:45.280 --> 0:39:48.279
<v Speaker 1>you know, it's it's something that could turn out to

0:39:48.360 --> 0:39:50.719
<v Speaker 1>be the case. I seriously doubt it, just based upon

0:39:50.760 --> 0:39:54.120
<v Speaker 1>the massive amounts of research and time that has been

0:39:54.160 --> 0:39:56.960
<v Speaker 1>dedicated to studying this already. It could be caused by

0:39:57.000 --> 0:40:03.960
<v Speaker 1>interdimensional reptiles. Okay, Tilly, sorry, so ignoring ignoring my co

0:40:04.080 --> 0:40:06.200
<v Speaker 1>hosts for the time being. Well, no, it's it's a

0:40:06.200 --> 0:40:09.200
<v Speaker 1>hoax they came up with to fund their war against

0:40:09.200 --> 0:40:15.080
<v Speaker 1>the Zeta reticulum. Attempting to continue to ignore my co hosts.

0:40:15.160 --> 0:40:19.239
<v Speaker 1>All right, So anyway, it'll be our next episode. We're

0:40:19.280 --> 0:40:23.399
<v Speaker 1>really going to be focusing on how best to address this,

0:40:23.840 --> 0:40:25.919
<v Speaker 1>you know, assuming that all of the science is right,

0:40:26.160 --> 0:40:29.400
<v Speaker 1>which I think is well within our rights to assume,

0:40:29.440 --> 0:40:32.919
<v Speaker 1>because of the mass of probability that it is right.

0:40:33.520 --> 0:40:36.400
<v Speaker 1>What can we do to reduce our impact on the

0:40:36.520 --> 0:40:41.000
<v Speaker 1>environment and try and mitigate climate change. We're gonna talk

0:40:41.040 --> 0:40:43.880
<v Speaker 1>about that in our next episode. Now, I'm sure some

0:40:43.920 --> 0:40:45.640
<v Speaker 1>of you listeners out there have a lot that you

0:40:45.680 --> 0:40:48.160
<v Speaker 1>want to say about this topic. I recommend you go

0:40:48.239 --> 0:40:51.560
<v Speaker 1>to fw thinking dot com. That's our website where all

0:40:51.640 --> 0:40:55.880
<v Speaker 1>of our stuff lives. We're talking the videos, the blogs, podcasts, articles,

0:40:56.280 --> 0:40:59.880
<v Speaker 1>join in the conversation. You can follow us on Twitter, Facebook,

0:41:00.040 --> 0:41:02.520
<v Speaker 1>Google Plus just look for f W thinking We are

0:41:02.560 --> 0:41:06.200
<v Speaker 1>there as well. And meanwhile, we're gonna take a little break.

0:41:07.080 --> 0:41:09.040
<v Speaker 1>Let this room cool down a bit. It's been warming up.

0:41:09.080 --> 0:41:11.160
<v Speaker 1>I don't know if that's climate or whether or it's

0:41:11.200 --> 0:41:14.680
<v Speaker 1>just you don't Oh well, you know it's so sweet

0:41:14.880 --> 0:41:21.440
<v Speaker 1>and we will talk to you again. Really sorry. For

0:41:21.600 --> 0:41:24.400
<v Speaker 1>more on this topic in the future of technology, visit

0:41:24.440 --> 0:41:38.560
<v Speaker 1>forward thinking dot Com, brought to you by Toyota. Let's

0:41:38.600 --> 0:41:39.280
<v Speaker 1>Go Places