1 00:00:01,920 --> 00:00:06,360 Speaker 1: Welcome to brain Stuff production of I Heart Radio. Hey 2 00:00:06,440 --> 00:00:10,440 Speaker 1: brain Stuff, Lauren Bogabam. Here, I'm looking up into the sky, 3 00:00:10,720 --> 00:00:13,200 Speaker 1: be it a cloudy day or bright clear night with 4 00:00:13,280 --> 00:00:16,880 Speaker 1: the stars shining down. It may seem like Earth's atmosphere 5 00:00:16,960 --> 00:00:20,760 Speaker 1: is a single solid mass, but our sky is more 6 00:00:20,840 --> 00:00:24,120 Speaker 1: like a lasagna or maybe a trifle, with layers that 7 00:00:24,200 --> 00:00:27,000 Speaker 1: ripple up and down depending on what's beneath them, and 8 00:00:27,120 --> 00:00:31,840 Speaker 1: merge into each other in different and interesting ways. And today, though, 9 00:00:32,000 --> 00:00:36,320 Speaker 1: let's talk about the layer called the stratosphere. But first, 10 00:00:36,640 --> 00:00:40,559 Speaker 1: we're all creatures of the troposphere. This atmosphere layer is 11 00:00:40,560 --> 00:00:43,400 Speaker 1: where almost all of the weather related phenomena on planet 12 00:00:43,400 --> 00:00:46,880 Speaker 1: Earth unfold. Although the troposphere begins at the surface of 13 00:00:46,920 --> 00:00:50,680 Speaker 1: our planet, its upper boundary is less consistent, and depending 14 00:00:50,720 --> 00:00:53,639 Speaker 1: on your latitude and the current season, the layer's top 15 00:00:53,720 --> 00:00:56,440 Speaker 1: might be located anywhere from four to seven miles that's 16 00:00:56,440 --> 00:01:01,320 Speaker 1: seven to twelve kilometers overhead. Above the troposphere. We have 17 00:01:01,600 --> 00:01:07,360 Speaker 1: in order the stratosphere, mesisphere, thermosphere, and exosphere. But let's 18 00:01:07,360 --> 00:01:09,319 Speaker 1: go back and talk about those first two layers more. 19 00:01:10,800 --> 00:01:16,000 Speaker 1: The troposphere stratosphere boundary or tropopause separates two areas with 20 00:01:16,160 --> 00:01:21,319 Speaker 1: inverted temperature trends. Inside the troposphere, the global average temperature 21 00:01:21,440 --> 00:01:25,360 Speaker 1: decreases as you go higher, and yet it's a different 22 00:01:25,400 --> 00:01:28,240 Speaker 1: story in the stratosphere, where things get warmer as you 23 00:01:28,280 --> 00:01:32,319 Speaker 1: go higher. Eventually you'll hit the stratosphere's ceiling some thirty 24 00:01:32,319 --> 00:01:35,840 Speaker 1: miles or fifty kilometers up. Beyond that point, the trend 25 00:01:35,880 --> 00:01:39,520 Speaker 1: starts to reverse itself. Things get pretty chilly in the mesisphere. 26 00:01:41,120 --> 00:01:44,399 Speaker 1: You've probably visited the stratosphere once or twice at least. 27 00:01:45,120 --> 00:01:47,960 Speaker 1: The region's hard to avoid for anyone who travels by 28 00:01:48,000 --> 00:01:52,600 Speaker 1: air frequented by commercial airlines. The stratosphere is also a 29 00:01:52,640 --> 00:01:56,480 Speaker 1: bastion of ozone gas and rapid winds, where clouds are 30 00:01:56,480 --> 00:02:02,400 Speaker 1: scarce but life indoors. The scientists have found microorganisms adrift 31 00:02:02,440 --> 00:02:05,920 Speaker 1: in the stratosphere. Participants in a study published in August 32 00:02:06,360 --> 00:02:10,200 Speaker 1: eighteen in the journal Frontiers and Microbiology designed and built 33 00:02:10,280 --> 00:02:13,959 Speaker 1: an air capturing probe that was installed on a NASA plane. 34 00:02:14,440 --> 00:02:18,520 Speaker 1: The gadget detected bacteria whizzing around above the local tropopause 35 00:02:18,720 --> 00:02:24,320 Speaker 1: at altitudes of seven miles or twelve kilometers. UV radiation 36 00:02:24,400 --> 00:02:27,480 Speaker 1: and extreme temperatures make the stratosphere a rough place for 37 00:02:27,560 --> 00:02:31,320 Speaker 1: living things to survive up there. Some bacteria depend on 38 00:02:31,440 --> 00:02:36,120 Speaker 1: sun blocking pigments and protective outer shells. Fast DNA repair 39 00:02:36,320 --> 00:02:39,760 Speaker 1: is another life saving trick. Hitching rides on storms and 40 00:02:39,840 --> 00:02:45,840 Speaker 1: volcanic eruptions. Microbes used the stratosphere as an atmospheric super highway. There, 41 00:02:46,240 --> 00:02:49,760 Speaker 1: winds carry them across the continents at great speeds, allowing 42 00:02:49,760 --> 00:02:53,600 Speaker 1: the microbes to disperse. The fact that life can tolerate 43 00:02:53,600 --> 00:02:57,480 Speaker 1: our stratosphere, even for limited periods, could profoundly impact the 44 00:02:57,560 --> 00:03:03,440 Speaker 1: hunt for, for example, Martian organism. But speaking of life, 45 00:03:03,919 --> 00:03:07,120 Speaker 1: other stuff in the stratosphere makes most life on Earth possible. 46 00:03:08,080 --> 00:03:12,320 Speaker 1: Ozone gas safeguards this planet from excessive ultraviolet or UV 47 00:03:12,560 --> 00:03:16,000 Speaker 1: radiation that's sent to us by the Sun. Made up 48 00:03:16,000 --> 00:03:20,200 Speaker 1: of oxygen atoms, ozone, like many sunscreens, absorbs UV light. 49 00:03:21,120 --> 00:03:24,240 Speaker 1: Entire ecosystems would fail if not for that critical service. 50 00:03:25,040 --> 00:03:27,880 Speaker 1: Our atmosphere supply of the gas is mostly limited to 51 00:03:27,880 --> 00:03:31,720 Speaker 1: the famous ozone layer, and about this layer is contained 52 00:03:31,720 --> 00:03:36,400 Speaker 1: within the stratosphere. On a related note, the ozone explains 53 00:03:36,440 --> 00:03:41,360 Speaker 1: why stratospheric temperatures climb at higher altitudes. Not only does 54 00:03:41,400 --> 00:03:44,400 Speaker 1: it absorb the Sun's UV rays, but it also soaks 55 00:03:44,480 --> 00:03:48,960 Speaker 1: up infrared radiation from the troposphere. The result a stratosphere 56 00:03:49,000 --> 00:03:54,840 Speaker 1: that grows toastier by the mile. Okay, so the troposphere 57 00:03:54,960 --> 00:03:59,520 Speaker 1: is cloud city, but be they stratos or cumulonimbus. You 58 00:03:59,600 --> 00:04:04,080 Speaker 1: need water droplets and or ice crystals to make clouds, 59 00:04:04,120 --> 00:04:08,240 Speaker 1: So the relatively wet troposphere is a great environment for them, 60 00:04:08,240 --> 00:04:11,760 Speaker 1: but the stratosphere not so much. By and large, it's 61 00:04:11,840 --> 00:04:16,719 Speaker 1: just too dry to facilitate cloud formation. Still, that cloud 62 00:04:16,720 --> 00:04:21,040 Speaker 1: shortage isn't a bad thing. The stratosphere combines largely cloud 63 00:04:21,080 --> 00:04:26,239 Speaker 1: free skies with limited turbulence, making it attractive to airline pilots. Indeed, 64 00:04:26,320 --> 00:04:29,840 Speaker 1: most commercial planes hit their cruising altitudes in the lower stratosphere. 65 00:04:30,880 --> 00:04:34,520 Speaker 1: When stratospheric clouds do form, they're sometimes created by the 66 00:04:34,560 --> 00:04:38,919 Speaker 1: mixing of ice with volcanic dust. Also the polar regions 67 00:04:38,920 --> 00:04:43,440 Speaker 1: see stratosphere level clouds during the wintertime. That's because the 68 00:04:43,440 --> 00:04:47,320 Speaker 1: stratosphere is also home to the Arctic seasonal polar vortex, 69 00:04:47,839 --> 00:04:51,440 Speaker 1: a huge swirling cyclone with a pocket of super cold 70 00:04:51,480 --> 00:04:55,520 Speaker 1: air on the inside caused by the big temperature contrast 71 00:04:55,560 --> 00:04:59,160 Speaker 1: of air over the pole versus warmer air from lower latitudes. 72 00:05:00,040 --> 00:05:04,360 Speaker 1: The vortex collapses every spring and reforms every winter, trapping 73 00:05:04,440 --> 00:05:08,240 Speaker 1: the coldest air right around the pole. We've been hearing 74 00:05:08,240 --> 00:05:10,560 Speaker 1: a lot about it the past few years because many 75 00:05:10,600 --> 00:05:13,360 Speaker 1: scientists think that due to climate change and warmer than 76 00:05:13,440 --> 00:05:18,240 Speaker 1: usual temperatures, the stratospheric polar vortex is weakening, allowing those 77 00:05:18,320 --> 00:05:26,880 Speaker 1: ultra cold winds that it normally traps head south. Today's 78 00:05:26,880 --> 00:05:29,880 Speaker 1: episode is based on the article the Stratosphere where birds 79 00:05:29,880 --> 00:05:32,840 Speaker 1: and planes fly and bacteria thrives on how stuff works 80 00:05:32,839 --> 00:05:36,039 Speaker 1: dot Com, written by Mark Mancini. Brain Stuff is production 81 00:05:36,080 --> 00:05:38,039 Speaker 1: of I Heart Radio in partnership with how stuff Works 82 00:05:38,080 --> 00:05:40,800 Speaker 1: dot Com and is produced by Tyler Clang. Four more 83 00:05:40,800 --> 00:05:44,480 Speaker 1: podcasts my heart Radio, visit the heart Radio app, Apple Podcasts, 84 00:05:44,560 --> 00:05:46,359 Speaker 1: or wherever you listen to your favorite shows