1 00:00:02,970 --> 00:00:06,707 [music playing] 2 00:00:06,707 --> 00:00:08,242 - Hi, I'm Mishay for "NASA eClips," 3 00:00:08,242 --> 00:00:10,110 and today I'm at the Virginia Living Museum 4 00:00:10,110 --> 00:00:11,945 in Newport News, Virginia. 5 00:00:11,945 --> 00:00:13,947 Today I'll be talking with some NASA scientists 6 00:00:13,947 --> 00:00:16,316 to learn more about how scientists gather information 7 00:00:16,316 --> 00:00:18,018 about Earth systems. 8 00:00:18,018 --> 00:00:23,023 [music playing] 9 00:00:29,096 --> 00:00:30,364 I'm here with Jessica Taylor 10 00:00:30,364 --> 00:00:32,132 from NASA Langley Research Center. 11 00:00:32,132 --> 00:00:34,801 Jessica is an atmospheric scientist. 12 00:00:34,801 --> 00:00:36,303 - Hi, Mishay. It's nice to meet you. 13 00:00:36,303 --> 00:00:37,905 - It's nice to meet you too. 14 00:00:37,905 --> 00:00:39,306 - I understand that you want to learn more about how NASA 15 00:00:39,306 --> 00:00:41,742 scientists gather information about our earth. 16 00:00:41,742 --> 00:00:43,277 - That's right. 17 00:00:43,277 --> 00:00:45,112 For my science class, I learned that Earth is a part 18 00:00:45,112 --> 00:00:46,914 of one big system, but it also is a part 19 00:00:46,914 --> 00:00:48,615 of some smaller subsystems. 20 00:00:48,615 --> 00:00:50,784 But I'm not quite sure how all that works together. 21 00:00:50,784 --> 00:00:53,687 - Well, why don't we go inside and go to cypress swamp 22 00:00:53,687 --> 00:00:56,256 and I can show you a little more about how these Earth systems 23 00:00:56,256 --> 00:00:58,559 interact. 24 00:00:58,559 --> 00:01:01,562 As you can see, the Earth really is a complex system. 25 00:01:01,562 --> 00:01:02,996 Changes in one part of the subsystem 26 00:01:02,996 --> 00:01:04,831 can impact the whole planet. 27 00:01:04,831 --> 00:01:06,266 Scientists study the Earth system 28 00:01:06,266 --> 00:01:08,302 by looking at multiple spheres. 29 00:01:08,302 --> 00:01:11,471 The water here is an example of the hydrosphere. 30 00:01:11,471 --> 00:01:15,843 The air that we breathe is an example of the atmosphere. 31 00:01:15,843 --> 00:01:17,110 The land that you see here, 32 00:01:17,110 --> 00:01:19,346 that's an example of the lithosphere. 33 00:01:19,346 --> 00:01:20,881 And all of these animals-- 34 00:01:20,881 --> 00:01:23,083 the turtles, the fish, and the ducks, 35 00:01:23,083 --> 00:01:26,053 they're all part of the biosphere, living things. 36 00:01:26,053 --> 00:01:28,155 And then there's the cryosphere, ice. 37 00:01:28,155 --> 00:01:30,324 We can't see that here because we're in Virginia, 38 00:01:30,324 --> 00:01:32,226 and it just doesn't get cold enough here. 39 00:01:32,226 --> 00:01:33,794 Scientists keep an eye on these systems 40 00:01:33,794 --> 00:01:35,762 to make sure they're functioning as we expect. 41 00:01:35,762 --> 00:01:37,030 While scientists look at changes 42 00:01:37,030 --> 00:01:38,465 right here at our Earth's surface, 43 00:01:38,465 --> 00:01:40,300 NASA also uses satellites, 44 00:01:40,300 --> 00:01:42,769 with instruments looking back down at Earth from space. 45 00:01:42,769 --> 00:01:44,738 And we use these satellites to collect data 46 00:01:44,738 --> 00:01:47,674 for long-term global perspective. 47 00:01:47,674 --> 00:01:50,344 - So what kind of tools do you use to look at those changes? 48 00:01:50,344 --> 00:01:52,613 - Well, let's find out more by talking with a friend of mine, 49 00:01:52,613 --> 00:01:54,047 Dr. Steven Pawson. 50 00:01:54,047 --> 00:01:56,450 He's at NASA's Goddard Space Flight Center. 51 00:01:56,450 --> 00:01:57,751 So let's come right over here, 52 00:01:57,751 --> 00:01:59,586 and we can call Dr. Pawson directly. 53 00:02:02,022 --> 00:02:04,258 [keypad beeping] 54 00:02:04,258 --> 00:02:05,859 - Hi, Dr. Pawson. 55 00:02:05,859 --> 00:02:07,561 Jessica and I have already talked about Earth systems, 56 00:02:07,561 --> 00:02:09,930 but I don't understand how these systems affect climate 57 00:02:09,930 --> 00:02:12,165 or how NASA can track that. 58 00:02:12,165 --> 00:02:14,101 - Yes, I'm very happy to talk about that. 59 00:02:14,101 --> 00:02:15,836 First, what we know about climate 60 00:02:15,836 --> 00:02:19,439 is that it includes not only the temperature of Earth 61 00:02:19,439 --> 00:02:20,707 but also lots of other things, 62 00:02:20,707 --> 00:02:23,277 such as the cycles of carbon and water. 63 00:02:23,277 --> 00:02:25,078 Now, what does NASA do? 64 00:02:25,078 --> 00:02:27,648 Because NASA built satellites that can orbit Earth, 65 00:02:27,648 --> 00:02:30,417 it means we can see all places from space. 66 00:02:30,417 --> 00:02:32,719 This gives us a much bigger view that we can see 67 00:02:32,719 --> 00:02:34,321 from the surface alone. 68 00:02:34,321 --> 00:02:36,456 So the instruments on NASA's satellites 69 00:02:36,456 --> 00:02:38,892 help us see the complete Earth and also measure different parts 70 00:02:38,892 --> 00:02:40,594 of the climate system. 71 00:02:40,594 --> 00:02:42,763 - So, Steven, can you explain to Mishay 72 00:02:42,763 --> 00:02:45,032 a little more about the tools that are used 73 00:02:45,032 --> 00:02:46,266 to gather this kind of data? 74 00:02:46,266 --> 00:02:48,101 And then once NASA has the data, 75 00:02:48,101 --> 00:02:51,071 how is that data analyzed and visualized? 76 00:02:51,071 --> 00:02:52,806 - So I think what's very interesting 77 00:02:52,806 --> 00:02:55,008 is that usually when we're measuring from space, 78 00:02:55,008 --> 00:02:56,510 we're actually measuring the light 79 00:02:56,510 --> 00:02:58,212 that's coming into the satellite, 80 00:02:58,212 --> 00:03:01,014 whether that's light in the visible spectrum that we can 81 00:03:01,014 --> 00:03:02,850 or whether it's infrared or ultraviolet light 82 00:03:02,850 --> 00:03:04,585 that we can't see, but it's still part 83 00:03:04,585 --> 00:03:06,920 of the electromagnetic spectrum. 84 00:03:06,920 --> 00:03:08,622 And to make real use of these data, 85 00:03:08,622 --> 00:03:10,791 we have to be able to deduce the quantities 86 00:03:10,791 --> 00:03:12,125 that we're interested in. 87 00:03:12,125 --> 00:03:14,428 So we know that if we're looking for ice, 88 00:03:14,428 --> 00:03:16,063 then if there's a lot of ice, 89 00:03:16,063 --> 00:03:17,431 more light will be reflected; 90 00:03:17,431 --> 00:03:19,066 and if there's not much ice, 91 00:03:19,066 --> 00:03:20,701 it won't be reflected. 92 00:03:20,701 --> 00:03:22,703 So in a way that's a relatively straightforward measurement. 93 00:03:22,703 --> 00:03:24,605 We can detect if there is ice there or not. 94 00:03:24,605 --> 00:03:27,341 But typically, if we're trying to deduce the temperature 95 00:03:27,341 --> 00:03:28,942 of the Earth from space, 96 00:03:28,942 --> 00:03:31,011 then we're looking at a different part of the spectrum 97 00:03:31,011 --> 00:03:33,747 and we have to be able to separate impacts of temperature 98 00:03:33,747 --> 00:03:36,750 from water vapor and from other gases in the atmosphere 99 00:03:36,750 --> 00:03:39,920 and do what we call a retrieval of that information. 100 00:03:39,920 --> 00:03:43,123 And a retrieval is really using a lot of complex physical models 101 00:03:43,123 --> 00:03:46,460 to try to understand what it is that we're observing 102 00:03:46,460 --> 00:03:48,695 and what's causing the change in the light that we're measuring. 103 00:03:48,695 --> 00:03:51,899 Typically, the physical models are mathematical equations, 104 00:03:51,899 --> 00:03:55,369 but what we actually do is code them to run on a computer. 105 00:03:55,369 --> 00:03:58,172 Instead of reading just one column of the atmosphere, 106 00:03:58,172 --> 00:04:02,109 we're looking at a grid over the entire Earth of points, 107 00:04:02,109 --> 00:04:04,678 and that includes the atmosphere, the land, 108 00:04:04,678 --> 00:04:06,180 and the ocean. 109 00:04:06,180 --> 00:04:09,249 And when we know what the state is at any one time, 110 00:04:09,249 --> 00:04:11,151 we can run those models forward in time, 111 00:04:11,151 --> 00:04:12,986 using very, very powerful computers. 112 00:04:12,986 --> 00:04:15,956 And from those we can deduce what is going to happen 113 00:04:15,956 --> 00:04:17,624 in one day or two days. 114 00:04:17,624 --> 00:04:19,226 For instance, we can make weather forecasts 115 00:04:19,226 --> 00:04:20,794 or we can run climate projections, 116 00:04:20,794 --> 00:04:24,531 which are running up to about 100 years ahead. 117 00:04:24,531 --> 00:04:28,302 Using this technique, we're able to deduce 118 00:04:28,302 --> 00:04:30,337 a lot of information about the surface of Earth 119 00:04:30,337 --> 00:04:32,072 and the atmosphere, 120 00:04:32,072 --> 00:04:36,376 and even the surface layer of land and oceans from space. 121 00:04:36,376 --> 00:04:38,345 - Thank you so much to Dr. Steven Pawson 122 00:04:38,345 --> 00:04:39,813 and Jessica Taylor. 123 00:04:39,813 --> 00:04:41,715 Want to find out more about Earth systems 124 00:04:41,715 --> 00:04:44,551 and the work being done by NASA and other scientists? 125 00:04:44,551 --> 00:04:45,819 Go to this website. 126 00:04:45,819 --> 00:04:47,387 That's all for now. 127 00:04:47,387 --> 00:04:50,657 I'm Mishay, and I'll see you next time on "NASA eClips."