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