WEBVTT FILE 1 00:00:00.000 --> 00:00:01.380 2 00:00:01.400 --> 00:00:04.730 Nitrogen oxides and ozone measurement. 3 00:00:04.750 --> 00:00:06.410 It's built for this aircraft, 4 00:00:06.430 --> 00:00:07.240 recently, 5 00:00:07.260 --> 00:00:09.350 so these are its maiden flights. 6 00:00:09.370 --> 00:00:11.510 And we're measuring four different things 7 00:00:11.530 --> 00:00:13.880 simultaneously every 10th of a second 8 00:00:13.900 --> 00:00:14.830 in the atmosphere, 9 00:00:14.850 --> 00:00:18.980 so about every 100 feet as the aircraft travels. 10 00:00:19.000 --> 00:00:20.490 The things we emit, 11 00:00:20.510 --> 00:00:22.060 including these things down here 12 00:00:22.080 --> 00:00:23.310 that we're measuring, 13 00:00:23.330 --> 00:00:24.760 drive ozone photochemistry 14 00:00:24.780 --> 00:00:26.230 in the atmosphere. 15 00:00:26.250 --> 00:00:29.060 So power plants, tailpipes of cars, 16 00:00:29.080 --> 00:00:31.670 your backyard bar-b-que, forest fires, 17 00:00:31.690 --> 00:00:33.040 make these nitrogen oxides. 18 00:00:33.060 --> 00:00:34.470 They're reactive, 19 00:00:34.490 --> 00:00:36.340 and they cook along in the sunlight 20 00:00:36.360 --> 00:00:38.080 in the atmosphere to make ozone, 21 00:00:38.100 --> 00:00:39.620 as part of the ozone recipe. 22 00:00:39.640 --> 00:00:40.830 It's a pollutant 23 00:00:40.850 --> 00:00:42.250 and it affects people's health 24 00:00:42.270 --> 00:00:45.330 and it affects the viability of plants, 25 00:00:45.350 --> 00:00:49.250 and it's also a substantial greenhouse gas. 26 00:00:49.270 --> 00:00:52.110 It couples to both air quality and to climate. 27 00:00:52.130 --> 00:00:54.650 So this is how we try to look at our data. 28 00:00:54.670 --> 00:00:56.280 We flew up and down and up and down 29 00:00:56.300 --> 00:00:57.800 on this black trace. 30 00:00:57.820 --> 00:00:59.980 And the ozone has a vertical structure 31 00:01:00.000 --> 00:01:01.870 shown here in blue, 32 00:01:01.890 --> 00:01:03.780 and the nitrogen oxides we're measuring 33 00:01:03.800 --> 00:01:05.330 are shown here in red. 34 00:01:05.350 --> 00:01:07.880 You can see that very similarly, 35 00:01:07.900 --> 00:01:08.980 as we're heading south, 36 00:01:09.000 --> 00:01:11.030 going up and down, 37 00:01:11.050 --> 00:01:12.930 you kind of get this decrease 38 00:01:12.950 --> 00:01:14.680 as you get closer to the equator, 39 00:01:14.700 --> 00:01:15.830 and all of a sudden 40 00:01:15.850 --> 00:01:16.680 the ozone you see here 41 00:01:16.700 --> 00:01:17.410 and the ozone you see here 42 00:01:17.430 --> 00:01:19.770 is missing at the highest altitudes 43 00:01:19.790 --> 00:01:21.180 very close to the equator. 44 00:01:21.200 --> 00:01:23.320 The contrast between north and south 45 00:01:23.340 --> 00:01:24.930 is going to tell us a lot about 46 00:01:24.950 --> 00:01:27.330 how the large sources in the north, 47 00:01:27.350 --> 00:01:29.390 of human pollution, 48 00:01:29.410 --> 00:01:30.640 affect the global atmosphere 49 00:01:30.660 --> 00:01:33.780 differently in the south, with fewer sources, 50 00:01:33.800 --> 00:01:35.250 and different hemispheres 51 00:01:35.270 --> 00:01:37.250 will have different seasons as well. 52 00:01:37.270 --> 00:01:39.710 You see this really boring stretch down here, 53 00:01:39.730 --> 00:01:41.480 down south, close to the equator 54 00:01:41.500 --> 00:01:43.470 in Southern Hemispheric air. 55 00:01:43.490 --> 00:01:45.050 And that little line looks really flat, 56 00:01:45.070 --> 00:01:46.600 but if you zoom in, 57 00:01:46.620 --> 00:01:48.970 one of the many many things we're going to 58 00:01:48.990 --> 00:01:50.930 hope to be able to do with these data 59 00:01:50.950 --> 00:01:53.480 is to say how fast does this gas, 60 00:01:53.500 --> 00:01:56.310 this greenhouse gas, this pollutant gas, ozone, 61 00:01:56.330 --> 00:01:58.230 stick to the ocean surface 62 00:01:58.250 --> 00:01:59.690 and go away from the atmosphere. 63 00:01:59.710 --> 00:02:01.420 And that's a really key thing 64 00:02:01.440 --> 00:02:03.280 to get right in the global climate 65 00:02:03.300 --> 00:02:05.880 and global chemistry models. 66 00:02:05.900 --> 00:02:08.842