WEBVTT FILE 1 00:00:00.050 --> 00:00:04.080 [wind] 2 00:00:04.100 --> 00:00:08.130 [rain] As the Hurricane and Severe 3 00:00:08.150 --> 00:00:12.170 Storm Sentinel campaign takes off, the Global Hawk aircraft 4 00:00:12.190 --> 00:00:16.200 will serve as a long-distance airborne laboratory designed to study the factors 5 00:00:16.220 --> 00:00:20.230 that can create and drastically change tropical cyclones. 6 00:00:20.250 --> 00:00:24.270 This airborne mission-- 7 00:00:24.290 --> 00:00:28.290 HS3 for short--is studying those storms, and one of the 8 00:00:28.310 --> 00:00:32.310 targets of study is the Saharan Air Layer. 9 00:00:32.330 --> 00:00:36.340 This warm, dusty mass of air originates from the Sahara and 10 00:00:36.360 --> 00:00:40.370 drifts west into the Atlantic. The exact impact of the 11 00:00:40.390 --> 00:00:44.400 Saharan Air Layer is unclear. Research has shown that the SAL 12 00:00:44.420 --> 00:00:48.460 can weaken a storm by promoting downdrafts, and its 13 00:00:48.480 --> 00:00:52.500 strong winds can increase vertical wind shear in and around the storm. 14 00:00:52.520 --> 00:00:56.530 During the HS3 campaign, scientists will analyze the Saharan Air 15 00:00:56.550 --> 00:01:00.550 Layer using a suite of instruments on board the unmanned Global Hawk 16 00:01:00.570 --> 00:01:04.600 aircraft. One instrument, the Cloud Physics Lidar, 17 00:01:04.620 --> 00:01:08.650 will gather data straight through storms and dusty air layers. 18 00:01:08.670 --> 00:01:12.650 Braun: The Cloud Physics Lidar, or CPL, gives us the vertical profile 19 00:01:12.670 --> 00:01:16.690 of the dust. So we can see not only where within the atmosphere it is, but 20 00:01:16.710 --> 00:01:20.720 get a relative sense at least of how much dust there is 21 00:01:20.740 --> 00:01:24.750 and the extent to which it's getting wrapped into the storm circulation. 22 00:01:24.770 --> 00:01:28.770 The lidar works by sending 5,000 rapid light pulses a second 23 00:01:28.790 --> 00:01:32.810 that bounce and scatter off any particles they encounter. The light 24 00:01:32.830 --> 00:01:36.830 that bounces back to the instrument can help distinguish the type of particle, 25 00:01:36.850 --> 00:01:40.860 which then gives us a better look at the anatomy of the storm. 26 00:01:40.880 --> 00:01:44.900 Data from the Cloud Physics Lidar will not only improve models 27 00:01:44.920 --> 00:01:48.920 of the Saharan Air Layer, but also expand the understanding of how 28 00:01:48.940 --> 00:01:52.960 the dust interacts with the storms. Braun: That's really the measurement challenge 29 00:01:52.980 --> 00:01:57.020 is to be able to collect the needed observations 30 00:01:57.040 --> 00:02:01.050 of where the Saharan Air is, what its characteristics are, how 31 00:02:01.070 --> 00:02:05.080 much does it penetrate into a storm, and when it does, what 32 00:02:05.100 --> 00:02:09.140 is it actually doing to the storm? How is it inhibiting development? And those 33 00:02:09.160 --> 00:02:13.160 are things that we're trying to answer. 34 00:02:13.180 --> 00:02:17.200 [beeping, thunder] 35 00:02:17.220 --> 00:02:21.240 36 00:02:21.260 --> 00:02:25.250 37 00:02:25.270 --> 00:02:26.526