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.