1 00:00:00,010 --> 00:00:04,020 [Thunder] 2 00:00:04,040 --> 00:00:08,050 [Thunder] 3 00:00:08,070 --> 00:00:12,070 [Thunder] [Music] 4 00:00:12,090 --> 00:00:16,110 Deep within their roiling clouds, thunderstorms hold an elusive 5 00:00:16,130 --> 00:00:20,170 surprise. Under just the right conditions, they produce some of the highest 6 00:00:20,190 --> 00:00:24,250 energy radiation naturally found on Earth: terrestrial gamma-ray 7 00:00:24,270 --> 00:00:28,270 or TGFs for short. 8 00:00:28,290 --> 00:00:32,290 Studies by NASA's Fermi Gamma-ray Space Telescope 9 00:00:32,310 --> 00:00:36,320 have shown that TGFs fire up about 1,100 times a day. 10 00:00:36,340 --> 00:00:40,330 Now, new research combines Fermi detections 11 00:00:40,350 --> 00:00:44,360 with ground-based radar and lightning location data. 12 00:00:44,380 --> 00:00:48,380 These studies show that TGFs come from more diverse types of storms than previously thought 13 00:00:48,400 --> 00:00:52,410 In a thunderstorm, collisions among rain and snow cause different 14 00:00:52,430 --> 00:00:56,440 parts of the clouds to develop positive and negative electrical charges. 15 00:00:56,460 --> 00:01:00,470 When the strength of the electric field overcomes the insulating properties in 16 00:01:00,490 --> 00:01:04,480 the thundercloud, a lighting flash occurs. 17 00:01:04,500 --> 00:01:08,500 Most lightning occurs entirely within the cloud and is called an intracloud flash. 18 00:01:08,520 --> 00:01:12,530 All lightning produces a strong and sudden change in the storm's electric field, 19 00:01:12,550 --> 00:01:16,540 but the upward portion of an intracloud flash sometimes sends a surge 20 00:01:16,560 --> 00:01:20,570 of electrons rushing toward the upper part of the storm. Reaching 21 00:01:20,590 --> 00:01:24,600 speeds nearly as fast as light, these accelerated electrongs give off 22 00:01:24,620 --> 00:01:28,610 gamma rays when their paths are deflected by air molecules. Using 23 00:01:28,630 --> 00:01:32,640 global lightning location networks, scientists can determine a TGF 24 00:01:32,660 --> 00:01:36,680 position more accurately than with Fermi data alone. Two dozen 25 00:01:36,700 --> 00:01:40,690 localized TGFs occurred within areas covered by next-generation weather 26 00:01:40,710 --> 00:01:44,710 radar systems. This gives scientists the opportunity to begin studying 27 00:01:44,730 --> 00:01:48,750 the kinds of storms that produce TGFs. These slices of 28 00:01:48,770 --> 00:01:52,770 radar data capture different types of storms encompassing a wide range of 29 00:01:52,790 --> 00:01:56,780 updraft strengths. Even the weakest of them produced a TGF. 30 00:01:56,800 --> 00:02:00,830 Another finding: TGFs seem to occur 31 00:02:00,850 --> 00:02:04,840 in the same altitude range, between 7 and 9 miles high. 32 00:02:04,860 --> 00:02:08,860 Lightning can form at much lower altitudes, so there's every reason 33 00:02:08,880 --> 00:02:12,940 to think TGFs can too, but gamma-rays from TGFs occuring 34 00:02:12,960 --> 00:02:16,960 deeper in the atmosphere are greatly weekend, they're too dim for Fermi to detect, 35 00:02:16,980 --> 00:02:21,020 which probably means the satellite is undercounting them. 36 00:02:21,040 --> 00:02:25,050 TGFs may be far more common than we think. With this 37 00:02:25,070 --> 00:02:29,080 knowledge, scientists can design experiments to track storms and 38 00:02:29,100 --> 00:02:33,140 study how TGFs relate to their strength and evolution. This will give us 39 00:02:33,160 --> 00:02:37,240 an even better understanding of planet Earth's most powerful natural particle 40 00:02:37,260 --> 00:02:41,270 accelerator. [Beeping] 41 00:02:41,290 --> 00:02:45,310 [Beeping and thunder] 42 00:02:45,330 --> 00:02:49,016 [Thunder]