WEBVTT FILE 1 00:00:00.934 --> 00:00:04.537 Where we are today, think of as the box of eight crayons, 2 00:00:04.904 --> 00:00:07.440 and you can do a lot of amazing things with that. 3 00:00:07.774 --> 00:00:11.578 So the information content for any singular 4 00:00:11.578 --> 00:00:14.314 instrument on PACE is way more than we're used to. 5 00:00:14.748 --> 00:00:18.885 OCI is going to be the box of 96 or 128 crayons. 6 00:00:18.885 --> 00:00:22.622 And so suddenly the tools you have at your fingertips will fill 7 00:00:22.622 --> 00:00:25.125 in all the gaps of color that we could possibly want. 8 00:00:25.125 --> 00:00:30.063 This observatory is going to provide global coverage every day. 9 00:00:30.463 --> 00:00:35.468 That is another scale of this total volume that is really, really increasing 10 00:00:35.735 --> 00:00:38.705 the amount of information we have to work with. 11 00:00:38.705 --> 00:00:41.674 [music] 12 00:00:41.741 --> 00:00:44.244 We know the atmosphere is changing. 13 00:00:44.244 --> 00:00:47.414 We know carbon dioxide levels have increased. 14 00:00:47.881 --> 00:00:50.350 We know that has warmed our atmosphere. 15 00:00:50.350 --> 00:00:52.719 Circulation patterns are changing. 16 00:00:53.253 --> 00:00:55.755 Places are warmer than they used to be. 17 00:00:56.189 --> 00:01:00.026 The deeper dive we take into the relationships 18 00:01:00.026 --> 00:01:02.796 between land, ocean and atmosphere, 19 00:01:03.063 --> 00:01:05.799 the more we realize we don't know and we need to learn. 20 00:01:06.266 --> 00:01:09.569 NASA is preparing to take that deeper dive with the Plankton, 21 00:01:09.569 --> 00:01:13.173 Aerosol, Cloud, ocean Ecosystem mission, or PACE. 22 00:01:13.673 --> 00:01:15.675 The PACE mission and its suite of instruments 23 00:01:15.675 --> 00:01:19.212 will gather new data on these interconnected Earth systems. 24 00:01:21.347 --> 00:01:24.250 The exchange of carbon between the oceans, land and atmosphere. 25 00:01:24.851 --> 00:01:29.055 The impacts of atmospheric particles on marine communities of phytoplankton. 26 00:01:29.422 --> 00:01:32.592 The changes these communities are experiencing in a warmer Earth. 27 00:01:33.326 --> 00:01:36.996 Reducing the uncertainty of aerosols and scientific climate models. 28 00:01:37.497 --> 00:01:40.934 PACE will improve our understanding of these complex connections 29 00:01:41.134 --> 00:01:45.105 and how these systems are affected in a changing climate. 30 00:01:45.105 --> 00:01:47.140 [music] 31 00:01:47.140 --> 00:01:51.544 The color of the oceans can tell us a lot about our changing Earth systems, 32 00:01:51.544 --> 00:01:54.514 but there's much more to it than just what the eye can see. 33 00:01:54.781 --> 00:01:58.418 And so PACE carries the Ocean Color Instrument, or OCI, 34 00:01:58.418 --> 00:02:01.754 to continuously measure the interaction of sunlight with substances 35 00:02:01.754 --> 00:02:05.959 in seawater, such as the green photosynthetic pigment chlorophyll-a. 36 00:02:06.726 --> 00:02:07.527 We're very good 37 00:02:07.527 --> 00:02:11.297 today at saying there's a lot of green, meaning there are a lot of plants. 38 00:02:11.297 --> 00:02:15.735 Where we want to go with OCI is what kind of plant is actually there. 39 00:02:15.735 --> 00:02:18.738 And so by looking at more color, you can actually start 40 00:02:18.738 --> 00:02:21.841 getting the subtleties of this green versus 41 00:02:21.841 --> 00:02:23.409 the slightly different shade of green 42 00:02:23.409 --> 00:02:26.613 and then relate that to the composition of what you're looking at. 43 00:02:27.046 --> 00:02:30.350 To measure very subtle differences in shades of any color, 44 00:02:30.350 --> 00:02:33.920 OCI needs to measure light at much finer wavelength resolutions 45 00:02:33.920 --> 00:02:36.523 than any other NASA sensor. 46 00:02:37.123 --> 00:02:39.092 From the sea to sky, 47 00:02:39.092 --> 00:02:42.795 PACE’s other two instruments are multiangle polarimeters, 48 00:02:42.795 --> 00:02:46.299 one hyperspectral and the other hyperangular. 49 00:02:46.299 --> 00:02:50.470 Together, they'll take on aerosols, tiny airborne particles, and clouds, 50 00:02:50.770 --> 00:02:54.240 both of which change how sunlight interacts with the atmosphere. 51 00:02:54.240 --> 00:03:00.413 So by those two polarimeters keeping their eyes on our home planet 52 00:03:00.413 --> 00:03:03.783 all of the time, because they're making measurements on global scales, 53 00:03:03.783 --> 00:03:08.288 we'll have a much better sense of general evolving 54 00:03:08.288 --> 00:03:12.625 air quality on multiple local, regional and global scales. 55 00:03:13.026 --> 00:03:16.496 With very few exceptions, we not only make these data available 56 00:03:16.496 --> 00:03:21.434 in rapid semi-real time, but we've developed tools 57 00:03:21.434 --> 00:03:25.872 that are open source that allow anybody who wishes of accessing these data 58 00:03:25.872 --> 00:03:27.774 and coming to their own conclusions. 59 00:03:28.675 --> 00:03:29.943 The data from PACE will help 60 00:03:29.943 --> 00:03:34.080 scientists reveal complex relationships that connect the atmosphere, ocean 61 00:03:34.080 --> 00:03:38.051 and land in ways that help explain changes we see in our own lives 62 00:03:38.318 --> 00:03:42.722 and in ways that impact generations to come. 63 00:03:42.722 --> 00:03:45.692 [music]