WEBVTT FILE 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