WEBVTT FILE 1 00:00:00.180 --> 00:00:04.190 [ rain, thunder ] 2 00:00:04.210 --> 00:00:08.220 [ thunder, music ] 3 00:00:08.240 --> 00:00:12.250 [ bugs buzzing ] If we measure the Earth from the ground, we 4 00:00:12.270 --> 00:00:16.280 can a get a good local picture of what is going around us. 5 00:00:16.300 --> 00:00:20.330 But if we want to measure larger portions of the Earth, then we'll need to use 6 00:00:20.350 --> 00:00:24.360 remote sensing. Remote 7 00:00:24.380 --> 00:00:28.400 sensing measures the Earth and its features without making physical contact. 8 00:00:28.420 --> 00:00:32.430 We can gather data from entire continents over longer time 9 00:00:32.450 --> 00:00:36.460 periods so we can look at how the Earth is changing. 10 00:00:36.480 --> 00:00:40.540 NASA uses specialized aircraft and sophisticated satellites to gather 11 00:00:40.560 --> 00:00:44.580 data using both passive and active remote sensing methods. 12 00:00:44.600 --> 00:00:48.700 Passive remote sensing measures the natural energy, or radiation, of the 13 00:00:48.720 --> 00:00:52.810 Earth. Active remote sensing gathers data by actively sending 14 00:00:52.830 --> 00:00:56.870 out signals that interact with the target of interest. 15 00:00:56.890 --> 00:01:00.900 Using both active and passive remote sensing techniques, NASA can look at 16 00:01:00.920 --> 00:01:04.960 soil moisture maps to monitor drought, estimate 17 00:01:04.980 --> 00:01:09.030 snowpack in areas where snow is crucial for freshwater, 18 00:01:09.050 --> 00:01:13.090 measure the change in ice sheets and sea level, tracking 19 00:01:13.110 --> 00:01:17.140 storms that could impact human lives, and observing how 20 00:01:17.160 --> 00:01:21.200 precipitation changes affect where we get our freshwater. The Global 21 00:01:21.220 --> 00:01:25.230 Precipitation Measurement mission helps fill in the gaps where ground measurement 22 00:01:25.250 --> 00:01:29.260 isn't enough. Places with rugged terrain can block the signals from ground 23 00:01:29.280 --> 00:01:33.310 radars. The oceans are too vast to cover with enough 24 00:01:33.330 --> 00:01:37.340 ships and measurement stations on the surface, and places 25 00:01:37.360 --> 00:01:41.390 without the network of instruments needed to measure freshwater for people and agriculture. 26 00:01:41.410 --> 00:01:45.450 We can then unify the measurements to create a consistent and 27 00:01:45.470 --> 00:01:49.510 accurate picture no matter where we are. Because satellites get 28 00:01:49.530 --> 00:01:53.560 more complete coverage than ground-based instruments, we can use remote sensing 29 00:01:53.580 --> 00:01:57.600 to better see how the whole Earth is changing over time. 30 00:01:57.620 --> 00:02:01.720 With a long data record we can make better predictions about the water cycle, the climate, 31 00:02:01.740 --> 00:02:05.830 and the impact on humans. [ wind, thunder, rain ] 32 00:02:05.850 --> 00:02:09.900 [ wind, debris flying ] 33 00:02:09.920 --> 00:02:13.970 [ tree splitting, insects swarming ] 34 00:02:13.990 --> 00:02:18.020 [ debris falling, bubbling, airplanes ] 35 00:02:18.040 --> 00:02:22.050 [ music ] 36 00:02:22.070 --> 00:02:26.100 By observing our Earth from above, we get a much better understanding of what is happening 37 00:02:26.120 --> 00:02:30.160 on the surface, in the atmosphere, 38 00:02:30.180 --> 00:02:34.200 underground, over the globe, and in our own 39 00:02:34.220 --> 00:02:38.230 backyard. [ music ] 40 00:02:38.250 --> 00:02:39.006