1 00:00:00,000 --> 00:00:04,050 When it comes to hurricanes, research has come a long 2 00:00:04,070 --> 00:00:08,110 way to help predict when and where a storm will hit. 3 00:00:08,130 --> 00:00:12,160 Forecasting intensity is a much bigger challenge, and 4 00:00:12,180 --> 00:00:16,210 an instrument called HIWRAP will investigate the strength of a storm. 5 00:00:16,230 --> 00:00:20,250 The HIWRAP instrument will fly aboard an aircraft to study storms 6 00:00:20,270 --> 00:00:24,280 from the very large down to the very small scale. Braun: And because those smaller 7 00:00:24,300 --> 00:00:28,330 scales tend to be much chaotic and difficult to predict, 8 00:00:28,350 --> 00:00:32,350 and the interactions between those smaller scales and the large scales is far more 9 00:00:32,370 --> 00:00:36,350 complex, it makes it a huge challenge to try to 10 00:00:36,370 --> 00:00:40,410 improve intensity forecasts. The High-Altitude Imaging 11 00:00:40,430 --> 00:00:44,500 Wind and Rain Airborne Profiler, or HIWRAP, is a 12 00:00:44,520 --> 00:00:48,560 radar designed to examine the factors of storm intensity. 13 00:00:48,580 --> 00:00:52,610 Braun: The HIWRAP Doppler radar is a dual-frequency radar, so it has two frequencies 14 00:00:52,630 --> 00:00:56,650 that measure at two different angles and as the plane is 15 00:00:56,670 --> 00:01:00,700 flying, it's sort of scanning in a cone. 16 00:01:00,720 --> 00:01:04,730 And as it's flying over a particular target--say, the eyewall of a storm--by scanning 17 00:01:04,750 --> 00:01:08,750 in a cone it looks first one way, and then sees the storm from a different direction. 18 00:01:08,770 --> 00:01:12,760 And that's what allows us then to measure the three-dimensional 19 00:01:12,780 --> 00:01:16,850 winds and precipitation within the storm. Because the storm and the aircraft 20 00:01:16,870 --> 00:01:20,920 are both moving, the HIWRAP must send out 5,000 pulses 21 00:01:20,940 --> 00:01:24,980 a second to get an accurate read on precipitation particles, 22 00:01:25,000 --> 00:01:29,040 like rain or ice. The signals that bounce back reveal the type, 23 00:01:29,060 --> 00:01:33,090 size, and distribution of rain or ice particles, as well as 24 00:01:33,110 --> 00:01:37,130 how fast the particles are moving. The speed of the particles can help determine 25 00:01:37,150 --> 00:01:41,160 the wind and circulation in a storm. HIWRAP will provide 26 00:01:41,180 --> 00:01:45,210 scientists with years of unprecedented data that will allow them to 27 00:01:45,230 --> 00:01:49,220 decipher the formation, structure, and intensification 28 00:01:49,240 --> 00:01:53,300 of hurricanes. 29 00:01:53,320 --> 00:01:57,380 30 00:01:57,400 --> 00:02:01,440 31 00:02:01,460 --> 00:02:05,450 32 00:02:05,470 --> 00:02:05,472