1 00:00:00,600 --> 00:00:04,004 Narration: There is one place where we're seeing climate change unfold faster 2 00:00:04,004 --> 00:00:05,338 than anywhere else on Earth. 3 00:00:05,338 --> 00:00:06,673 Here. 4 00:00:07,774 --> 00:00:10,310 In fact, temperatures in the Arctic and boreal regions 5 00:00:10,310 --> 00:00:13,747 are rising nearly four times as fast as those in the mid-latitudes. 6 00:00:14,214 --> 00:00:17,684 That's why NASA has teamed up with local partners to better understand 7 00:00:17,684 --> 00:00:20,520 the vulnerability and resilience of these ecosystems, 8 00:00:20,987 --> 00:00:24,457 while also gathering valuable data that will help future Earth-observing 9 00:00:24,457 --> 00:00:26,226 satellites. 10 00:00:26,226 --> 00:00:28,028 From space, air and on the ground, 11 00:00:28,328 --> 00:00:31,631 we'll see how scientists are piecing together the story of the Arctic - 12 00:00:31,931 --> 00:00:34,768 from how it is changing to what that means for our planet. 13 00:00:36,169 --> 00:00:39,672 Because, as they say, what happens in the Arctic doesn't stay in 14 00:00:39,672 --> 00:00:47,847 the Arctic. 15 00:00:51,851 --> 00:00:53,820 Radio Chatter: PPA is engaged 16 00:00:53,987 --> 00:00:55,889 Radio Chatter: And we're radiating. 17 00:00:55,889 --> 00:00:58,691 Narration: One of the best ways to track how an environment is changing 18 00:00:58,691 --> 00:01:00,593 is to observe it from above. 19 00:01:00,593 --> 00:01:01,261 But where weather 20 00:01:01,261 --> 00:01:04,664 and vegetation can make it difficult to see the ground with the naked eye, 21 00:01:05,131 --> 00:01:08,535 specialized radar can pierce the clouds to give us a crystal clear 22 00:01:08,535 --> 00:01:10,270 look at the landscape. 23 00:01:10,270 --> 00:01:13,006 This special device - weighing nearly 1,000 lbs - 24 00:01:13,339 --> 00:01:17,010 collects data about soil moisture, vegetation, permafrost 25 00:01:17,010 --> 00:01:19,579 and other environmental processes on the ground below. 26 00:01:19,879 --> 00:01:23,416 In fact, it's so precise that NASA developed a special system 27 00:01:23,416 --> 00:01:27,020 for pilots to fly the exact same flight path year after year 28 00:01:27,387 --> 00:01:31,024 to get an accurate reading as to how a landscape is changing over time. 29 00:01:31,091 --> 00:01:34,861 Dr. Hoy: So with the airborne data, we can target exactly where we want to go 30 00:01:34,861 --> 00:01:36,796 and exactly when we want to go there. 31 00:01:36,796 --> 00:01:40,166 And we get very high resolution data so we can have a really clear picture 32 00:01:40,166 --> 00:01:41,167 of what's on the ground. 33 00:01:41,167 --> 00:01:41,901 Narration: That's Dr. Liz Hoy, 34 00:01:41,901 --> 00:01:45,105 Senior Scientist for NASA's ABoVE Mission. 35 00:01:45,505 --> 00:01:49,042 ABoVE has spent the last seven years studying environmental changes 36 00:01:49,042 --> 00:01:50,577 in the Arctic and boreal regions. 37 00:01:51,511 --> 00:01:54,013 The mission uses satellite, airborne and ground data 38 00:01:54,013 --> 00:01:57,217 to get a complete picture of what is unfolding in these ecosystems. 39 00:01:57,951 --> 00:02:01,254 Dr. Hoy: So our satellite data gives us a very broad picture of what's happening 40 00:02:01,254 --> 00:02:02,956 all over the landscape. 41 00:02:02,956 --> 00:02:04,557 And then with our airborne data, 42 00:02:04,557 --> 00:02:08,528 we can target specific locations and times when we want to get imagery. 43 00:02:08,828 --> 00:02:11,831 And then we can compare both our satellite and our airborne data 44 00:02:11,831 --> 00:02:13,266 with what's happening on the ground. 45 00:02:13,266 --> 00:02:16,402 And we have teams actually out on the ground making measurements. 46 00:02:16,402 --> 00:02:17,971 And putting all that together 47 00:02:17,971 --> 00:02:21,641 is really where we get a lot of the power of what we're able to study. 48 00:02:22,308 --> 00:02:24,444 Narration: And it all gets put together in Alaska. 49 00:02:25,879 --> 00:02:26,646 On the ground, 50 00:02:26,646 --> 00:02:30,917 These large dishes are used to communicate with NASA's Earth-observing satellites. 51 00:02:31,618 --> 00:02:34,921 Here, the data is downloaded and made public, which helps 52 00:02:34,921 --> 00:02:39,159 scientists connect the dots between what we see from space to on the ground. 53 00:02:39,826 --> 00:02:41,928 But why are these dishes in Alaska? 54 00:02:41,928 --> 00:02:45,698 Dr. Meyer: So the reason why these stations, like ASF, are built in Alaska 55 00:02:46,566 --> 00:02:48,835 is because Earth-observing satellites, 56 00:02:49,202 --> 00:02:52,272 if you think of their orbits, they converge in the polar regions. 57 00:02:52,839 --> 00:02:57,177 So in Alaska, we can see the same satellite more often than in the lower 48. 58 00:02:57,777 --> 00:03:00,480 Narration: In fact, this facility is in the perfect position 59 00:03:00,480 --> 00:03:03,816 to receive data from one of NASA's latest Earth-observing missions. 60 00:03:04,417 --> 00:03:07,954 NISAR is an upcoming satellite that will be launched by NASA 61 00:03:07,954 --> 00:03:11,090 in collaboration with the Indian Space Research Organization. 62 00:03:11,324 --> 00:03:14,761 It will use radar similar to what is flown on NASA's airborne missions, 63 00:03:14,761 --> 00:03:19,199 like for ABoVE, to measure fine, centimeter- scale, changes in Earth's surface. 64 00:03:19,232 --> 00:03:23,069 Dr. Meyer: What's interesting and unique about NISAR is that it's going to cover the globe 65 00:03:23,236 --> 00:03:26,639 regularly every 12 days, and it's going to do it at a 66 00:03:27,006 --> 00:03:31,244 a wavelength or a frequency range, so-called L-band frequencies, 67 00:03:31,644 --> 00:03:34,013 that are very useful for doing Earth observations. 68 00:03:34,781 --> 00:03:38,551 L-band will allow us to study ecosystem changes 69 00:03:38,551 --> 00:03:42,322 and deformations of the Earth's surface with higher accuracy 70 00:03:42,655 --> 00:03:46,659 and better spatial coverage than we can with current systems in space. 71 00:03:47,227 --> 00:03:50,163 Narration: And in the Arctic, some of the most pronounced environmental 72 00:03:50,163 --> 00:03:54,901 changes satellites can observe are happening right down the road. 73 00:03:54,901 --> 00:03:56,536 And it all starts with this stuff. 74 00:03:57,804 --> 00:03:58,638 Permafrost is 75 00:03:58,638 --> 00:04:02,208 frozen Earth, be it ice, soil or even organic material 76 00:04:02,375 --> 00:04:04,577 that has been frozen for two or more years. 77 00:04:05,011 --> 00:04:06,112 Most of Alaska 78 00:04:06,112 --> 00:04:10,083 and northern Canada has permafrost beneath a thin, active layer of soil. 79 00:04:10,550 --> 00:04:13,987 Problem is, when permafrost does thaw, it can wreak havoc 80 00:04:13,987 --> 00:04:16,356 on infrastructure and upend ecosystems. 81 00:04:18,157 --> 00:04:21,127 Dr. Walter Anthony: Not all permafrost contains ice, but here in interior 82 00:04:21,127 --> 00:04:24,631 Alaska, we have frozen soils with massive amounts of ice. 83 00:04:24,631 --> 00:04:28,601 There are very large ice wedges - ice wedges as big as garages. 84 00:04:29,369 --> 00:04:31,471 And so when that ice melts, 85 00:04:31,671 --> 00:04:35,241 the ground surface collapses and the sinkholes can fill with water. 86 00:04:35,475 --> 00:04:39,178 When that happens, new little ponds form- thermokarst ponds. 87 00:04:39,379 --> 00:04:43,283 And as thermokarst ponds form, microbes in the soil feast 88 00:04:43,283 --> 00:04:47,687 on the newly thawed organic material, releasing methane into the atmosphere - 89 00:04:48,288 --> 00:04:51,824 an extremely potent, and flammable greenhouse gas. 90 00:04:52,525 --> 00:04:55,795 These newly formed thermokarst ponds give us an insight 91 00:04:55,795 --> 00:04:58,231 as to what is going to happen in the future. 92 00:04:58,231 --> 00:05:02,502 Dr. Walter Anthony: What we're seeing at this lake is that the emissions are ten times 93 00:05:02,502 --> 00:05:06,673 higher than the rest of the lakes and wetlands in the Arctic, 94 00:05:07,206 --> 00:05:10,376 and it's being fueled by thawing permafrost. 95 00:05:10,877 --> 00:05:15,448 Narration: Scientists are working with ABoVE and NASA's UAVSAR to study 96 00:05:15,448 --> 00:05:18,618 how these lakes are evolving as the climate continues to warm. 97 00:05:19,218 --> 00:05:22,622 But it's not just thawing permafrost that is reshaping the Arctic. 98 00:05:23,122 --> 00:05:24,457 It is also wildfire. 99 00:05:25,792 --> 00:05:26,392 In higher 100 00:05:26,392 --> 00:05:30,063 latitudes, forests are adapted to burn about once every century. 101 00:05:30,530 --> 00:05:33,166 But with warmer temperatures comes more fires. 102 00:05:33,933 --> 00:05:35,702 And why is this? 103 00:05:35,702 --> 00:05:39,305 Partially because of this stuff, called duff, forest debris 104 00:05:39,305 --> 00:05:44,143 that slowly builds up on the forest floor, about one inch every 17 years. 105 00:05:44,544 --> 00:05:47,513 And because of the cold winters, it doesn't decompose. 106 00:05:47,880 --> 00:05:49,282 Alison: It doesn't have roots. 107 00:05:49,282 --> 00:05:52,485 So it's completely dependent on relative humidity for moisture. 108 00:05:52,485 --> 00:05:55,988 So it actually dries very rapidly in warm, 109 00:05:55,988 --> 00:05:58,925 dry conditions like we often have here in the summer. 110 00:05:59,192 --> 00:06:03,329 Narration: Which means of warmer temperatures, duff becomes a potent fuel for fires. 111 00:06:03,963 --> 00:06:07,233 Alison: Most Alaskans are vulnerable to wildland fire. 112 00:06:07,233 --> 00:06:11,270 And with climate change, it seems that the imprint on 113 00:06:11,270 --> 00:06:14,941 the landscape is growing, and so more and more communities are vulnerable. 114 00:06:15,241 --> 00:06:18,811 Dr. Hoy: When a wildfire comes through, what we're really seeing is it's actually 115 00:06:18,811 --> 00:06:20,346 it's not just the trees that are burning, 116 00:06:20,346 --> 00:06:22,515 but it's the soil layer that's burning as well. 117 00:06:22,749 --> 00:06:25,752 And so when that fire comes through and it burns that soil layer, it's 118 00:06:25,752 --> 00:06:30,022 like you're taking off the lid of a cooler where everything is frozen below. 119 00:06:30,256 --> 00:06:33,393 And so as that soil comes off, then we start to see the ground 120 00:06:33,393 --> 00:06:35,661 start to thaw and permafrost is thawing there. 121 00:06:36,562 --> 00:06:38,931 And so as we see those changes happening, 122 00:06:39,265 --> 00:06:42,802 we're actually creating more climate change over time. 123 00:06:42,802 --> 00:06:46,506 So wildfires are releasing carbon gases into the atmosphere. 124 00:06:46,506 --> 00:06:49,575 And then as permafrost thaws, it too is releasing carbon 125 00:06:49,575 --> 00:06:53,613 gases into the air, which then can create warmer conditions 126 00:06:53,846 --> 00:06:56,682 which can allow for more wildfire and more thaw. 127 00:06:56,883 --> 00:07:00,787 So you really see this cycle that continues up in boreal forest 128 00:07:00,787 --> 00:07:04,023 and Arctic areas over time. 129 00:07:05,024 --> 00:07:07,693 Narration: So the bad news is that as human-caused climate 130 00:07:07,693 --> 00:07:10,830 change continues to impact the Arctic and boreal landscapes, 131 00:07:11,664 --> 00:07:14,834 those living both near and far will continue to feel its effects. 132 00:07:16,035 --> 00:07:19,372 But the good news is that there is a team of dedicated scientists, 133 00:07:19,372 --> 00:07:23,242 across a variety of disciplines, that are working together to give us 134 00:07:23,242 --> 00:07:26,612 a complete picture of these ecosystems and how they are changing. 135 00:07:28,014 --> 00:07:30,750 Because this collective knowledge is key to understanding 136 00:07:30,750 --> 00:07:41,627 how we can lessen our impact.