WEBVTT FILE 1 00:00:05.038 --> 00:00:06.039 If we were to see the 2 00:00:06.039 --> 00:00:08.475 world with polarization-sensitive eyes, 3 00:00:09.075 --> 00:00:10.643 the sky would not be blue. 4 00:00:11.611 --> 00:00:13.079 Grass would look gray. 5 00:00:13.380 --> 00:00:16.383 There would be all sorts of strange things that would be happening. 6 00:00:16.616 --> 00:00:18.551 What we reveal about 7 00:00:18.551 --> 00:00:20.820 the environment with polarization 8 00:00:20.820 --> 00:00:23.156 is really kind of another dimension of information. 9 00:00:25.091 --> 00:00:28.695 The PACE mission holds the keys to unlock that dimension 10 00:00:28.695 --> 00:00:30.930 with two toaster-sized instruments 11 00:00:30.930 --> 00:00:32.832 called polarimeters, 12 00:00:32.932 --> 00:00:36.736 and polarimeters like these measure the polarization of sunlight. 13 00:00:36.803 --> 00:00:41.341 Generally, sunlight has a combination of different directions. 14 00:00:41.341 --> 00:00:46.479 Polarization is some preference for an oscillation direction. 15 00:00:46.880 --> 00:00:49.449 The ability to detect the specific direction 16 00:00:49.449 --> 00:00:52.118 sunlight reflects back to PACE’s instruments 17 00:00:52.118 --> 00:00:53.553 will give us more information 18 00:00:53.553 --> 00:00:57.657 about clouds and tiny atmospheric particles called aerosols. 19 00:00:58.158 --> 00:01:01.895 The aerosols are really important to human health, 20 00:01:01.961 --> 00:01:05.131 so that's why we need to really quantify what is out there, 21 00:01:05.131 --> 00:01:08.401 like what type of aerosols there are and where they come from. 22 00:01:08.835 --> 00:01:12.372 Various interactions with light in the environment, 23 00:01:12.372 --> 00:01:17.677 scattering events off of particles or surfaces can impose some preference 24 00:01:17.677 --> 00:01:22.382 in the light that they reflect in terms of the polarization nature. 25 00:01:23.516 --> 00:01:24.717 The two multi-angle 26 00:01:24.717 --> 00:01:27.187 polarimeters were built by NASA's partners 27 00:01:27.187 --> 00:01:29.022 both here and abroad. 28 00:01:29.155 --> 00:01:32.025 The Hyper-Angular Rainbow Polarimeter #2, 29 00:01:32.025 --> 00:01:33.159 or HARP2, 30 00:01:33.159 --> 00:01:34.994 will measure atmospheric particles 31 00:01:34.994 --> 00:01:36.729 in one of its spectral channels 32 00:01:36.729 --> 00:01:38.765 in up to 60 viewing angles. 33 00:01:39.199 --> 00:01:40.800 Why so many angles? 34 00:01:40.934 --> 00:01:43.169 This is like a camera, like any other kind of camera. 35 00:01:43.169 --> 00:01:45.905 But instead of taking a picture at 36 00:01:45.905 --> 00:01:48.675 one particular geometry of what 37 00:01:48.675 --> 00:01:50.376 we would understand as light, 38 00:01:50.376 --> 00:01:53.179 it's looking at a scene from different angles. 39 00:01:53.246 --> 00:01:55.782 We will move the different angles 40 00:01:55.782 --> 00:01:58.251 to the one single location, 41 00:01:58.251 --> 00:01:58.918 and in that way 42 00:01:58.918 --> 00:02:02.555 we will collect the information at all the different angles. 43 00:02:02.755 --> 00:02:06.326 And those different angles contain information about 44 00:02:06.326 --> 00:02:08.228 what's present in the environment. 45 00:02:09.028 --> 00:02:11.965 For instance, all these angles from HARP2 can analyze 46 00:02:11.965 --> 00:02:14.033 the elusive cloud bow. 47 00:02:19.105 --> 00:02:21.207 Cloud bows are slightly distinct from a rainbow. 48 00:02:21.207 --> 00:02:24.544 Rainbow is light scattering off of rain droplets. 49 00:02:24.544 --> 00:02:26.980 Cloud bows is light scattering off of cloud droplets, which 50 00:02:26.980 --> 00:02:28.114 are a little bit smaller. 51 00:02:28.882 --> 00:02:29.916 By being able to 52 00:02:29.916 --> 00:02:33.019 observe cloud bows with polarization, 53 00:02:33.019 --> 00:02:36.723 if we very accurately measure the geometry in which this happens, 54 00:02:36.723 --> 00:02:41.528 the exact position of that cloud bow with respect to the Sun, in our observation, 55 00:02:41.528 --> 00:02:44.931 it tells us a lot about the size distribution of the cloud droplets. 56 00:02:44.998 --> 00:02:47.100 If we understand the size distribution of cloud droplets, 57 00:02:47.100 --> 00:02:50.270 we can understand things about the formation of clouds and how long 58 00:02:50.270 --> 00:02:53.606 they will persist if they're going to turn into precipitation or not. 59 00:02:53.673 --> 00:02:57.110 Polarization can also reveal the shape of sunglint, 60 00:02:57.110 --> 00:03:01.014 the pattern of sunlight reflecting directly off the ocean's surface. 61 00:03:01.648 --> 00:03:05.785 Sunglint patterns can tell us how rough or smooth the ocean's surface is, 62 00:03:06.152 --> 00:03:09.122 which can determine wind speed at the surface. 63 00:03:10.323 --> 00:03:12.358 Clouds also have an impact on climate. 64 00:03:12.358 --> 00:03:14.527 But the interaction between the two, 65 00:03:14.527 --> 00:03:15.995 there's many pathways in which aerosols 66 00:03:15.995 --> 00:03:17.397 can interact with clouds. 67 00:03:17.397 --> 00:03:20.400 Cloud droplets can form around aerosol particles more easily 68 00:03:20.567 --> 00:03:23.203 and other things that are going on in the local situation. 69 00:03:23.203 --> 00:03:26.673 That complexity of the interaction between the two is one of the largest sources 70 00:03:26.673 --> 00:03:29.142 of uncertainty in understanding our global climate, 71 00:03:29.142 --> 00:03:31.411 and that's why we're making these measurements. 72 00:03:31.411 --> 00:03:35.515 The data from PACE will allow researchers to tease out the species of aerosols, 73 00:03:35.515 --> 00:03:39.519 which will help fine tune climate models so they make better predictions. 74 00:03:40.253 --> 00:03:44.457 PACE’s other polarimeter, SPEXone, will tackle aerosol retrievals 75 00:03:44.557 --> 00:03:47.427 and give us precise measurements of the angle, degree 76 00:03:47.427 --> 00:03:49.696 and intensity of polarization. 77 00:03:50.196 --> 00:03:54.200 But processing the sheer volume of data has been its own mission. 78 00:03:54.234 --> 00:03:59.572 Each pixel of data the polarimeters measure covers about five kilometers square. 79 00:03:59.572 --> 00:04:04.077 In that space are hundreds—even thousands— of observations at different angles, 80 00:04:04.077 --> 00:04:06.746 wavelengths and state of polarization. 81 00:04:06.746 --> 00:04:09.415 In the course of one full day of orbits 82 00:04:09.415 --> 00:04:11.017 those pixels pile up. 83 00:04:11.017 --> 00:04:12.685 If you put them together, 84 00:04:12.685 --> 00:04:16.122 there will be more than ten million pixels. 85 00:04:16.122 --> 00:04:21.094 That's a huge challenge on both storage and the computational power. 86 00:04:21.094 --> 00:04:22.061 To meet that challenge, 87 00:04:22.061 --> 00:04:24.931 the PACE team has turned to a kind of machine learning 88 00:04:24.931 --> 00:04:27.600 called a neural network emulator. 89 00:04:27.600 --> 00:04:29.802 Even before PACE gathers any data, 90 00:04:29.802 --> 00:04:31.371 the emulator has been trained with 91 00:04:31.371 --> 00:04:33.506 millions of simulations of the possible 92 00:04:33.506 --> 00:04:36.409 atmospheric conditions in that one pixel. 93 00:04:37.443 --> 00:04:40.146 With this emulator, what would take an hour for one 94 00:04:40.146 --> 00:04:42.415 pixel is now a matter of milliseconds, 95 00:04:42.415 --> 00:04:44.717 allowing PACE to process a seemingly 96 00:04:44.717 --> 00:04:45.985 endless stream of data 97 00:04:45.985 --> 00:04:47.053 for the mission 98 00:04:47.053 --> 00:04:49.389 and atmospheric researchers all over. 99 00:04:50.056 --> 00:04:52.292 They will require a lot of measurement, 100 00:04:52.292 --> 00:04:56.562 especially if we can do that from a global scale with satellites 101 00:04:56.562 --> 00:04:59.666 so we know where they're coming from so we can trace their source. 102 00:04:59.666 --> 00:05:02.969 We probably can help to reduce its impact on human health.