WEBVTT FILE 1 00:00:00.000 --> 00:00:04.030 Now this is a familiar scene. 2 00:00:04.050 --> 00:00:08.050 The Sun's heat causes water 3 00:00:08.070 --> 00:00:12.070 from plants, lakes and oceans to turn from a liquid to a vapor. 4 00:00:12.090 --> 00:00:16.080 High in the atmosphere 5 00:00:16.100 --> 00:00:20.090 the water vapor then cools down and condenses from a gas 6 00:00:20.110 --> 00:00:24.150 back into a liquid. The liquid 7 00:00:24.170 --> 00:00:28.190 water then falls back to the surface in the form of rain, snow, ice, 8 00:00:28.210 --> 00:00:32.240 or hail. Water 9 00:00:32.260 --> 00:00:36.270 runs off into streams, lakes and oceans or is stored in the ground or 10 00:00:36.290 --> 00:00:40.300 in snowpack. 11 00:00:40.320 --> 00:00:44.320 This is the water cycle, and it describes 12 00:00:44.340 --> 00:00:48.340 how our most vital resource moves through the whole Earth system. 13 00:00:48.360 --> 00:00:52.360 But like most things in our world, when we 14 00:00:52.380 --> 00:00:56.370 look at the tiny parts that make up the whole, we can learn a lot more about the 15 00:00:56.390 --> 00:01:00.420 phenomena. Take 16 00:01:00.440 --> 00:01:04.440 the shape of a single raindrop. Small droplets of 17 00:01:04.460 --> 00:01:08.450 water in the atmosphere are spherical in shape due to the surface tension, or 18 00:01:08.470 --> 00:01:12.470 "skin," of the water molecules. As these droplets grow 19 00:01:12.490 --> 00:01:16.490 they become heavier and start to fall through the air. 20 00:01:16.510 --> 00:01:20.500 As they fall, the raindrop collides with other drops and continues to get 21 00:01:20.520 --> 00:01:24.510 bigger. These larger raindrops fall through the air faster. 22 00:01:24.530 --> 00:01:28.520 The wind resistance on the underside of the drop causes the bottom 23 00:01:28.540 --> 00:01:32.580 of the drop to flatten, resulting in a drop looking like a hamburger bun. 24 00:01:32.600 --> 00:01:36.630 As the drop continues to fall and grow, at some point, it becomes too 25 00:01:36.650 --> 00:01:40.670 large for the surface tension to hold it together, so the raindrop breaks 26 00:01:40.690 --> 00:01:44.710 apart into smaller spherical drops. Investigating the proceses 27 00:01:44.730 --> 00:01:48.740 we can't see with the naked eye is nothing new. Science and technology 28 00:01:48.760 --> 00:01:52.760 drive each other forward and often lead to insights and discoveries along the way. 29 00:01:52.780 --> 00:01:56.780 With the invention of high-speed photography, we finally saw 30 00:01:56.800 --> 00:02:00.800 the most basic elements of our watery planet in action. 31 00:02:00.820 --> 00:02:04.810 Understanding how a tiny 32 00:02:04.830 --> 00:02:08.860 raindrop falls through the atmosphere does more than debunk the myth that a 33 00:02:08.880 --> 00:02:12.960 raindrop falls like a teardrop. It actually makes a difference when it comes to 34 00:02:12.980 --> 00:02:17.000 measuring precipitation, in particular, for ground radars. 35 00:02:17.020 --> 00:02:21.040 Ground radars look at the sides of the raindrops and then estimate 36 00:02:21.060 --> 00:02:25.070 the vertical and horizontal size. A heavier flatter drop allows 37 00:02:25.090 --> 00:02:29.100 radars to identify heavier precipitation. In fact the two 38 00:02:29.120 --> 00:02:33.130 radars on board the GPM satellite can also measure drop sizes 39 00:02:33.150 --> 00:02:37.140 from space and so a more accurate look at raindrops gives us a more 40 00:02:37.160 --> 00:02:41.150 accurate look at how global rainfall is shaping up. 41 00:02:41.170 --> 00:02:45.160 42 00:02:45.180 --> 00:02:50.017