1 00:00:00,010 --> 00:00:04,060 The new GPM Microwave Imager, or GMI, produced 2 00:00:04,080 --> 00:00:08,110 unprecedented images of an extra-tropical cyclone in the Northwest 3 00:00:08,130 --> 00:00:12,150 Pacific Ocean, east of Japan, on March 10, 2014. 4 00:00:12,170 --> 00:00:16,190 The GMI measures the natural energy radiated by 5 00:00:16,210 --> 00:00:20,220 different precipitation in the form of brightness temperatures. 6 00:00:20,240 --> 00:00:24,240 The GMI produces a critical reference standard, which unifies all the member 7 00:00:24,260 --> 00:00:28,260 satellites of the GPM Constellation. The instrument 8 00:00:28,280 --> 00:00:32,270 has 13 channels, four more than onboard TRMM, and this 9 00:00:32,290 --> 00:00:36,300 greater sensitivity allows GPM to measure a greater variety of 10 00:00:36,320 --> 00:00:40,330 precipitation type and intensity. Each channel 11 00:00:40,350 --> 00:00:44,370 has a frequency range that can detect a different type of precipitation. 12 00:00:44,390 --> 00:00:48,410 The lower frequencies for moderate to heavy rain, 13 00:00:48,430 --> 00:00:52,440 the middle frequencies for a mix of rain and snow, 14 00:00:52,460 --> 00:00:56,480 and the higher frequencies for falling snow and ice. 15 00:00:56,500 --> 00:01:00,520 Scientific algorithms then translate the 16 00:01:00,540 --> 00:01:04,540 GMI's brightness temperature data into more meaningful products, such as 17 00:01:04,560 --> 00:01:08,560 rain rates. Because GPM's coverage extends beyond 18 00:01:08,580 --> 00:01:12,630 the tropics, measuring storms like these in the mid- and high-latitudes 19 00:01:12,650 --> 00:01:16,690 will improve and expand the global view of precipitation. 20 00:01:16,710 --> 00:01:20,740 [rain falling] 21 00:01:20,760 --> 00:01:24,790 [rain falling] 22 00:01:24,810 --> 00:01:28,820 23 00:01:28,840 --> 00:01:32,820 24 00:01:32,840 --> 00:01:32,840