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.