WEBVTT FILE 1 00:00:00.500 --> 00:00:02.168 What color is the ocean? 2 00:00:02.168 --> 00:00:02.836 Trick question. 3 00:00:02.836 --> 00:00:04.671 It's all kinds of colors. 4 00:00:04.671 --> 00:00:07.874 Blues, greens, reds, yellows and swirls of all of the above. 5 00:00:07.974 --> 00:00:11.678 And these colors can tell us a lot about what's going on just beneath the surface, 6 00:00:11.845 --> 00:00:15.181 what's thriving or changing, or could pose a threat. 7 00:00:15.281 --> 00:00:18.351 For over 20 years, NASA has been looking at the color of the ocean 8 00:00:18.351 --> 00:00:21.588 with technology that's, well, over 20 years old. 9 00:00:21.688 --> 00:00:24.991 And that has taught us a lot about the health of ocean ecosystems, 10 00:00:25.091 --> 00:00:27.794 but there are details we just can't see. 11 00:00:27.794 --> 00:00:32.298 Enter PACE, the Plankton, Aerosol, Cloud, ocean Ecosystem mission. 12 00:00:32.399 --> 00:00:33.700 PACE’s new instruments 13 00:00:33.700 --> 00:00:37.404 will look at our world's oceans, lakes and rivers in an entire rainbow's 14 00:00:37.404 --> 00:00:41.408 worth of color and beyond, giving us new insights into marine communities, 15 00:00:41.541 --> 00:00:44.577 the carbon cycle and climate studies. 16 00:00:44.677 --> 00:00:48.148 So let's take a look at the top five official best-ever 17 00:00:48.148 --> 00:00:50.483 ocean colors of all time. 18 00:00:54.687 --> 00:00:56.923 This is the open ocean. 19 00:00:56.923 --> 00:01:01.795 Here the oceans absorb the longer red wavelengths and scatters the blues 20 00:01:01.895 --> 00:01:05.698 In these vast stretches of deepest blues is where the tiniest of bacteria 21 00:01:05.765 --> 00:01:09.769 cycle and recycle nutrients in microbial loops. 22 00:01:09.836 --> 00:01:12.372 For example, the tiniest and most abundant, 23 00:01:12.372 --> 00:01:16.743 photosynthetic organism, Prochlorococcus, converts carbon dioxide 24 00:01:16.743 --> 00:01:21.181 into organic compounds and forms the base of the marine food web. 25 00:01:21.281 --> 00:01:24.317 These phytoplankton are eaten by tiny zooplankton, 26 00:01:24.417 --> 00:01:29.189 and then eaten by larger zooplankton, then smaller fish and so on, 27 00:01:29.255 --> 00:01:33.526 and then return the nutrients back through respiration and remineralization, 28 00:01:33.593 --> 00:01:36.529 which are then taken up by the tiny microbes. 29 00:01:36.529 --> 00:01:38.364 But here is where things are changing. 30 00:01:38.364 --> 00:01:41.367 These deep blues are getting greener with a warming climate. 31 00:01:41.534 --> 00:01:44.070 But exactly how and why is unclear. 32 00:01:44.070 --> 00:01:47.440 Despite some scientific theories, The past and present satellite 33 00:01:47.440 --> 00:01:51.144 sensors just don't have enough sensitivity to color to tease that out. 34 00:01:51.244 --> 00:01:55.582 PACE will fill in those gaps with higher spectral information, and slowly 35 00:01:55.582 --> 00:02:00.954 over time be able to discern the drivers associated with these detected changes. 36 00:02:01.754 --> 00:02:03.423 This appealing brownish orange 37 00:02:03.423 --> 00:02:07.293 is the result of what's known as colored dissolved organic matter. 38 00:02:07.393 --> 00:02:10.663 We can think of it as a kind of tea that leaches out of dead or 39 00:02:10.663 --> 00:02:14.567 dying organic matter, like the tannins from broken down leaves, 40 00:02:14.634 --> 00:02:18.037 giving the surrounding water a darker, browner hue. 41 00:02:18.138 --> 00:02:22.142 Found in higher concentrations in lakes, rivers, estuaries and marshes 42 00:02:22.142 --> 00:02:25.411 colored dissolved organic matter is a great proxy for dissolved 43 00:02:25.411 --> 00:02:28.882 organic carbon, a big pool of carbon in aquatic systems, 44 00:02:29.015 --> 00:02:31.951 and it's an indicator of the health of an ecosystem. 45 00:02:31.951 --> 00:02:33.920 Much like a cloudy cup of tea, 46 00:02:33.920 --> 00:02:37.790 higher levels of this organic matter don't let as much light through, changing 47 00:02:37.790 --> 00:02:41.895 the availability of light for plant-like organisms in the environment. 48 00:02:41.995 --> 00:02:45.498 With PACE’s Ocean Color Instrument’s hyperspectral measurements, 49 00:02:45.565 --> 00:02:50.069 even into the ultraviolet wavelengths, we’ll be able to differentiate sources 50 00:02:50.069 --> 00:02:52.372 of this organic matter and better understand 51 00:02:52.372 --> 00:02:56.242 the transfer of carbon across land and into coastal regions. 52 00:02:57.043 --> 00:03:00.780 A grayish green in a large lake like this could spell potential harm 53 00:03:00.780 --> 00:03:04.651 from a bloom of blue-green algae known as cyanobacteria. 54 00:03:04.717 --> 00:03:08.054 Depending on the type and abundance, cyanobacteria can spread 55 00:03:08.054 --> 00:03:11.758 toxins to aquatic and human life. 56 00:03:11.858 --> 00:03:15.295 In 2019, Lake Erie saw a bloom of the Microcystis 57 00:03:15.295 --> 00:03:19.332 cyanobacteria form a thick layer of scum filled with a toxin, 58 00:03:19.399 --> 00:03:23.036 which posed a major risk to drinkable water. 59 00:03:23.102 --> 00:03:25.305 The Microcystin toxin can cause liver 60 00:03:25.305 --> 00:03:28.474 damage, dizziness, numbness and vomiting. 61 00:03:28.575 --> 00:03:32.312 Researchers are eager to use the hyperspectral information from PACE in 62 00:03:32.312 --> 00:03:37.584 order to detect early stages of harmful algal blooms, like the ones in Lake Erie. 63 00:03:37.684 --> 00:03:42.155 PACE will be able to measure the unique optical properties of cyanobacteria, 64 00:03:42.222 --> 00:03:46.092 which will help separate the harmful algae from other phytoplankton present 65 00:03:46.092 --> 00:03:50.997 in the water and allow resource managers to monitor the health of freshwater. 66 00:03:52.131 --> 00:03:55.034 This turquoise stretch tells us a lot about the sediment 67 00:03:55.034 --> 00:03:58.171 churning in the water, and both the quality and quantity 68 00:03:58.171 --> 00:04:01.641 of that sediment can have big impacts on marine life. 69 00:04:01.741 --> 00:04:05.378 For example, in Greenland, glaciers can bulldoze over surface rocks, 70 00:04:05.478 --> 00:04:11.084 grinding them into a fine powder of silt and clay, known as glacial flour. 71 00:04:11.184 --> 00:04:14.020 The glacial flour changes the appearance of the water, 72 00:04:14.020 --> 00:04:17.757 with the particles absorbing the shorter wavelengths, purples and indigos, 73 00:04:17.857 --> 00:04:21.961 and the water absorbing the longer wavelengths, the reds and oranges. 74 00:04:22.028 --> 00:04:25.632 This sediment can bring nutrients and fuel algal blooms, 75 00:04:25.732 --> 00:04:29.702 But if you're an oyster, sediments could be a big problem. 76 00:04:29.769 --> 00:04:32.905 When lots of sediment is suspended in the water, filter 77 00:04:32.905 --> 00:04:35.908 feeders like oysters can't feed as efficiently. 78 00:04:36.009 --> 00:04:41.247 And high sediment levels can be associated with increased harmful Vibrio bacteria, 79 00:04:41.347 --> 00:04:45.818 which can cause sickness and even death when those oysters are eaten. 80 00:04:45.918 --> 00:04:47.053 PACE’s hyperspectral 81 00:04:47.053 --> 00:04:50.456 measurements will see far more variability in reflectance 82 00:04:50.523 --> 00:04:54.060 and give us better estimates of water, clarity and particle size. 83 00:04:54.127 --> 00:04:56.996 And that data could be used by oyster farmers monitoring 84 00:04:56.996 --> 00:04:59.365 the health of the shellfish population. 85 00:05:00.900 --> 00:05:03.670 As the days grow longer in the subpolar regions, 86 00:05:03.670 --> 00:05:08.107 a milky swirly light blue hue grows in the oceans. 87 00:05:08.207 --> 00:05:10.910 This is the telltale mark of coccolithophores-- 88 00:05:10.910 --> 00:05:11.911 coccolithophores? 89 00:05:11.911 --> 00:05:14.380 Coccolithophores, a kind of phytoplankton 90 00:05:14.380 --> 00:05:18.384 that is completely covered in a chalky shell of calcium carbonate. 91 00:05:18.484 --> 00:05:21.054 When these plankton bloom and then die off, 92 00:05:21.054 --> 00:05:24.724 that inorganic chalky material sinks to the ocean floor. 93 00:05:24.791 --> 00:05:27.560 PACE will better observe these particular blooms, 94 00:05:27.560 --> 00:05:31.230 allowing researchers to account for the amount of carbon coccolithophores 95 00:05:31.230 --> 00:05:35.601 remove from the atmosphere and sink into the depths of the ocean. 96 00:05:36.669 --> 00:05:37.470 If all of these 97 00:05:37.470 --> 00:05:41.441 colors can tell us what's going on with our ecosystems, our health, 98 00:05:41.541 --> 00:05:46.179 our climate, then PACE’s enhanced resolution is going to reveal new levels 99 00:05:46.179 --> 00:05:50.350 of detail in how humans and water are connected in a changing world.