1 00:00:01,480 --> 00:00:12,320 ♪ 2 00:00:12,720 --> 00:00:15,920 >>Our planet is a living example of a delicate balance 3 00:00:16,480 --> 00:00:19,160 a complex system that is constantly changing, 4 00:00:19,160 --> 00:00:22,520 constantly evolving, constantly adapting. 5 00:00:28,160 --> 00:00:30,720 How do these changes affect life on Earth? 6 00:00:31,240 --> 00:00:34,160 How does everyday life affect our planet? 7 00:00:55,040 --> 00:00:59,080 We have a great capability to absorb, interpret and comprehend 8 00:00:59,080 --> 00:01:02,360 And an urge to understand the world we live in. 9 00:01:03,920 --> 00:01:06,840 This is what defines us as human beings... 10 00:01:06,840 --> 00:01:08,840 What makes us who we are. 11 00:01:15,000 --> 00:01:17,080 With our technological advancements 12 00:01:17,080 --> 00:01:20,640 we are now capable of exploring new worlds, new frontiers. 13 00:01:21,880 --> 00:01:24,720 We're searching for answers that may lay in front of us... 14 00:01:24,720 --> 00:01:26,880 Better yet... above us! 15 00:01:30,520 --> 00:01:33,400 The field phase of the experiment is about to begin. 16 00:01:33,400 --> 00:01:37,600 All the planning, sleepless nights, meetings and hard work 17 00:01:37,600 --> 00:01:40,360 the team has invested in the mission are at stake. 18 00:01:42,840 --> 00:01:44,800 My name is Jasna Pittman, 19 00:01:44,800 --> 00:01:47,320 and I'm one of the many scientists working on 20 00:01:47,320 --> 00:01:50,600 the Airborne Tropical Tropopause Experiment (ATTREX) 21 00:01:55,200 --> 00:01:56,720 >>It is very natural for humans 22 00:01:56,720 --> 00:01:59,920 to want to understand how the world around us works. 23 00:01:59,920 --> 00:02:02,320 >>Why the atmosphere does what it does? 24 00:02:02,320 --> 00:02:04,400 It's like solving a puzzle! 25 00:02:04,400 --> 00:02:07,720 >>You just want to understand how it works. 26 00:02:09,840 --> 00:02:12,800 >>We're trying to understand how we're affecting, 27 00:02:12,800 --> 00:02:15,000 how humans are affecting the atmosphere. 28 00:02:15,000 --> 00:02:17,440 >>Understanding how the stratosphere changes 29 00:02:17,440 --> 00:02:21,160 very much reflects how our climate is changing. 30 00:02:27,320 --> 00:02:30,160 >>I think that the work that is done in atmospheric science 31 00:02:30,160 --> 00:02:33,640 is very important! But it's also a lot of fun! 32 00:02:33,640 --> 00:02:37,000 >>It's like the best job possible! 33 00:02:45,200 --> 00:02:49,360 ♪ 34 00:02:56,800 --> 00:02:59,760 >>NASA has been doing airborne science investigations 35 00:02:59,760 --> 00:03:01,480 for quite some time. 36 00:03:01,480 --> 00:03:04,520 Some of the earliest investigations we were doing 37 00:03:04,520 --> 00:03:08,960 was related to the early days of the Antarctic ozone hole. 38 00:03:08,960 --> 00:03:15,920 >>In 2009 we started a new program called the Earth Venture Program. 39 00:03:15,920 --> 00:03:18,800 It's got three parts; and the first of those parts 40 00:03:18,800 --> 00:03:21,960 is what we call sub-orbital science. 41 00:03:21,960 --> 00:03:29,560 this is science done not including a new satellite. 42 00:03:42,960 --> 00:03:45,120 >>With some of these newer missions 43 00:03:45,120 --> 00:03:47,960 we have let the community come up with their own ideas, 44 00:03:47,960 --> 00:03:50,080 their own way of implementing the mission, 45 00:03:50,080 --> 00:03:52,120 what their own science requirements are 46 00:03:52,120 --> 00:03:54,280 and they bring their measurements to the table. 47 00:03:54,280 --> 00:03:58,680 >>And ATTREX had very good science, 48 00:03:58,680 --> 00:04:03,640 was very relevant to the kind of questions we wanted answered, 49 00:04:03,640 --> 00:04:07,600 and its budget was reasonable and appropriate. 50 00:04:23,160 --> 00:04:27,640 >>So ATTREX is an airborne campaign to try to understand 51 00:04:27,640 --> 00:04:32,160 how stratospheric water vapor affects climate. 52 00:04:32,160 --> 00:04:36,200 >>It causes perhaps, maybe, 15 to 20 percent 53 00:04:36,200 --> 00:04:40,760 of the warming that we've had in the past 15 or 20 years. 54 00:04:45,440 --> 00:04:49,200 >>It turns out that small changes in humidity in the stratosphere 55 00:04:49,200 --> 00:04:53,200 are very important for climate and for surface temperature. 56 00:04:53,200 --> 00:04:56,080 They are actually comparable to the importance 57 00:04:56,080 --> 00:04:58,920 of greenhouse gases that everybody knows about. 58 00:05:00,920 --> 00:05:06,440 >>So we know that carbon dioxide was less 30 years ago. 59 00:05:06,440 --> 00:05:09,880 Methane was less 30 years ago. 60 00:05:09,880 --> 00:05:12,640 Nitrous oxide was less 30 years ago. 61 00:05:12,640 --> 00:05:15,480 So we know these gases are increasing with time. 62 00:05:15,480 --> 00:05:18,000 >>Gases that affect the chemistry of the stratosphere 63 00:05:18,000 --> 00:05:20,400 which is where the ozone layer exists 64 00:05:20,400 --> 00:05:23,040 and protects us from ultraviolet radiation. 65 00:05:23,040 --> 00:05:26,120 >>So understanding the rate at which this stuff 66 00:05:26,120 --> 00:05:28,880 gets into the stratosphere and how it changes 67 00:05:28,880 --> 00:05:31,440 is extremely important to looking at the climate 68 00:05:31,440 --> 00:05:33,880 of the stratosphere and how the stratosphere climate affects 69 00:05:33,880 --> 00:05:35,520 the lower atmosphere. 70 00:05:35,800 --> 00:05:37,080 >>So we really need to understand 71 00:05:37,080 --> 00:05:40,840 what controls the humidity of the stratosphere 72 00:05:40,840 --> 00:05:43,720 and actually be able to predict that in the future 73 00:05:43,720 --> 00:05:46,760 in order to improve the accuracy 74 00:05:46,760 --> 00:05:50,080 of our predictions of future climate change. 75 00:05:57,000 --> 00:06:00,360 And it turns out that the most important place to go sample 76 00:06:00,360 --> 00:06:03,760 to understand that, is the tropical upper troposphere. 77 00:06:03,760 --> 00:06:07,680 The top of the troposphere in the tropics is called 78 00:06:07,680 --> 00:06:11,000 the "tropopause" which is actually at a very high-altitude 79 00:06:11,000 --> 00:06:14,680 which is why we need a high altitude aircraft to study it. 80 00:06:18,800 --> 00:06:20,560 >>So the tropical tropopause 81 00:06:20,560 --> 00:06:25,000 is at about 55,000 feet in the tropics. 82 00:06:25,000 --> 00:06:27,720 So if you go down to the equator you have to go up quite high 83 00:06:27,720 --> 00:06:29,320 above 50,000 feet. 84 00:06:29,320 --> 00:06:33,280 And the tropical tropopause is really important to the global atmosphere 85 00:06:33,280 --> 00:06:36,960 because most of the gases that get into the stratosphere, 86 00:06:36,960 --> 00:06:39,760 all the air that is circulating upward into the stratosphere, 87 00:06:39,760 --> 00:06:42,720 goes through this tropical tropopause region. 88 00:06:43,120 --> 00:06:45,600 >>So that is basically a gateway to the stratosphere. 89 00:06:45,600 --> 00:06:49,360 General circulation transports air upward in the tropics, 90 00:06:49,360 --> 00:06:51,240 goes into the stratosphere, 91 00:06:51,240 --> 00:06:53,520 and then spread throughout the stratosphere 92 00:06:53,520 --> 00:06:57,080 and comes down at the higher latitudes in the polar regions. 93 00:06:57,080 --> 00:06:59,200 >>And this is what ATTREX is focused on, 94 00:06:59,200 --> 00:07:02,960 to look at that motion of air into the stratosphere 95 00:07:02,960 --> 00:07:05,440 and how the water is removed 96 00:07:05,440 --> 00:07:08,000 from that air as it rises upward. 97 00:07:08,000 --> 00:07:11,040 >>We know a lot about it, but there are some puzzles 98 00:07:11,040 --> 00:07:14,120 about the details of how the clouds form, 99 00:07:14,120 --> 00:07:16,280 and under what conditions they form. 100 00:07:16,280 --> 00:07:18,400 So that's probably the most important thing 101 00:07:18,400 --> 00:07:21,120 that we hope to gain from ATTREX. 102 00:07:24,360 --> 00:07:28,400 >>ATTREX will address a number of really important issues. 103 00:07:28,400 --> 00:07:31,480 It'll give us a better understanding of the exchange 104 00:07:31,480 --> 00:07:33,960 between the troposphere and stratosphere 105 00:07:33,960 --> 00:07:37,080 and how that impacts atmospheric composition. 106 00:07:37,080 --> 00:07:40,880 How that affects the chemistry in the upper atmosphere. 107 00:07:40,880 --> 00:07:42,400 And, in the longer term, 108 00:07:42,400 --> 00:07:44,320 how that will affect the climate. 109 00:07:44,320 --> 00:07:48,720 >>And that will help us to understand as we go forward 110 00:07:48,720 --> 00:07:52,040 trying to figure out what to do about climate change 111 00:07:52,040 --> 00:07:55,160 to better predict it and make better decisions. 112 00:08:10,800 --> 00:08:13,520 >>How does the interaction between the upper troposphere 113 00:08:13,520 --> 00:08:16,360 and the lower stratosphere affects us down below? 114 00:08:16,920 --> 00:08:18,680 How are we going to find out? 115 00:08:19,560 --> 00:08:21,040 We have the questions.