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