WEBVTT FILE 1 00:00:01.810 --> 00:00:05.980 [ no audio ] 2 00:00:06.000 --> 00:00:10.000 3 00:00:10.020 --> 00:00:14.010 4 00:00:14.030 --> 00:00:18.190 5 00:00:18.210 --> 00:00:22.210 Sure, what we need to understand 6 00:00:22.230 --> 00:00:26.400 you know, not just what's happening in our backyard, but also what's happening at the global 7 00:00:26.420 --> 00:00:30.430 scale, and because we're able to observe both light rain and heavy 8 00:00:30.450 --> 00:00:34.440 rain and snow. We're able to see how storm systems that originate in our part 9 00:00:34.460 --> 00:00:38.640 of the world, for example Hurricane Bertha, you know we can see how that affects 10 00:00:38.660 --> 00:00:42.650 other places. So Hurricane Bertha was not such an interesting storm for 11 00:00:42.670 --> 00:00:46.840 the U.S. but as it moved across the Atlantic it caused 12 00:00:46.860 --> 00:00:50.960 extensive flooding and actually some fatalities in the United Kingdom. 13 00:00:50.980 --> 00:00:54.980 So getting that global picture and being able to track patterns of weather from 14 00:00:55.000 --> 00:00:59.170 one place to another is a very powerful way to see how our water cycle 15 00:00:59.190 --> 00:01:03.180 and our weather is interconnected. 16 00:01:03.200 --> 00:01:07.380 17 00:01:07.400 --> 00:01:11.460 18 00:01:11.480 --> 00:01:15.030 It took about ten years to build the satellite and we have some great 19 00:01:15.050 --> 00:01:19.110 video showing how the instruments were added to the space spacecraft bus 20 00:01:19.130 --> 00:01:22.730 how they were tested, how we shipped the spacecraft 21 00:01:22.750 --> 00:01:26.740 From the United States, NASA Goddard Space Flight Center 22 00:01:26.760 --> 00:01:30.750 To Tanegashima Island in Japan, our partners with this satellite. 23 00:01:30.770 --> 00:01:34.760 But really the concept for this mission was about 10 years prior 24 00:01:34.780 --> 00:01:38.780 to that. So really from concept to launch was almost 25 00:01:38.800 --> 00:01:42.780 20 years. so it takes a long time to conceive. build. and launch 26 00:01:42.800 --> 00:01:48.710 such a satellite. 27 00:01:48.730 --> 00:01:54.600 28 00:01:54.620 --> 00:01:56.720 Well knowing where when and how 29 00:01:56.740 --> 00:02:00.900 much it's raining and snowing is really vital for understanding extreme events like 30 00:02:00.920 --> 00:02:04.960 landslides or floods. You know one of the things that we observed is that there's 31 00:02:04.980 --> 00:02:08.960 different seasons for some of these intense hazards that can cause fatalities. 32 00:02:08.980 --> 00:02:12.970 For example the monsoon season in Asia, for example 33 00:02:12.990 --> 00:02:16.990 can cause extensive landsliding. Every August and September and October 34 00:02:17.010 --> 00:02:21.160 we have lots of landslides and flooding as a result 35 00:02:21.180 --> 00:02:25.220 of heavy rains from the monsoons. In other areas we have 36 00:02:25.240 --> 00:02:29.230 flooding from the spring rains or from heavy summer rains 37 00:02:29.250 --> 00:02:33.430 So it really depends on what season is and what the 38 00:02:33.450 --> 00:02:37.440 the topography of the areas that can cause both strange weather and 39 00:02:37.460 --> 00:02:41.620 impacts like natural disasters. 40 00:02:41.640 --> 00:02:45.810 41 00:02:45.830 --> 00:02:49.830 42 00:02:49.850 --> 00:02:54.010 Understanding how our water cycle is connected 43 00:02:54.030 --> 00:02:58.200 so where air moves and evaporates 44 00:02:58.220 --> 00:03:02.230 from the surface, it condenses to cause precipitation and where that goes 45 00:03:02.250 --> 00:03:06.240 whether it's over land or over ocean really tells us about what 46 00:03:06.260 --> 00:03:10.430 our reservoir in the sky is doing and how that feeds our reservoir 47 00:03:10.450 --> 00:03:14.450 on the surface and underground. And so with satellites we get 48 00:03:14.470 --> 00:03:18.150 this remote perspective allowing us to see the whole globe at once. 49 00:03:18.170 --> 00:03:22.840 You know if you look at water gauges for example, we don't have any over the oceans. 50 00:03:22.860 --> 00:03:25.360 But what you can see in this rainfall accumulation 51 00:03:25.380 --> 00:03:29.370 showing this Super Tyhoon Haglong is that 52 00:03:29.390 --> 00:03:33.390 we have a ton of rainfall over the ocean and then also it impacts land. 53 00:03:33.410 --> 00:03:37.410 and caused extensive flooding in Japan. And so if you take all of the 54 00:03:37.430 --> 00:03:41.590 rain gauges in the world and put them together they only fit into two basketball courts. So we really 55 00:03:41.610 --> 00:03:45.600 need that vantage point of space to tell us what's happening with our 56 00:03:45.620 --> 00:03:49.650 precipitation and where it might impact society. 57 00:03:49.670 --> 00:03:53.680 58 00:03:53.700 --> 00:03:57.690 59 00:03:57.710 --> 00:04:01.720 Well Earth is a very interesting system. We have 60 00:04:01.740 --> 00:04:05.790 this very, very tropical warm region which 61 00:04:05.810 --> 00:04:09.890 evaporates water from the surface and it condenses and it creates 62 00:04:09.910 --> 00:04:14.020 a lot of rain in the tropics. Now when you move farther up that air 63 00:04:14.040 --> 00:04:18.090 moves up and sinks at the kind of middle latitudes in the deserts and 64 00:04:18.110 --> 00:04:22.100 This is where we see most of the Earth's deserts in the Sahara, but 65 00:04:22.120 --> 00:04:26.130 also over the ocean. There's actually a desert over the ocean. 66 00:04:26.150 --> 00:04:30.180 If you look at areas that get a lot of rainfall, you know there's sometimes where, 67 00:04:30.200 --> 00:04:34.200 the fissures get really wet. You know we have these huge areas where 68 00:04:34.220 --> 00:04:38.230 you have a lot of freshwater coming into our oceans. And then higher up, 69 00:04:38.250 --> 00:04:42.270 we have, for example, light rainfall which is a huge contributer 70 00:04:42.290 --> 00:04:46.290 to freshwater resources in high latitudes. So that circling 71 00:04:46.310 --> 00:04:50.320 of and cycling of precipitation both from 72 00:04:50.340 --> 00:04:54.360 land to ocean as well as from the equator to the poles 73 00:04:54.380 --> 00:04:58.390 is important and vital for driving our global water cycle 74 00:04:58.410 --> 00:05:02.430 and our global energy cycle. And so that's why understanding precipitation 75 00:05:02.450 --> 00:05:06.490 where it is, how much we have and where it's moving is so important. 76 00:05:06.510 --> 00:05:10.490 77 00:05:10.510 --> 00:05:14.500 78 00:05:14.520 --> 00:05:18.540 79 00:05:18.560 --> 00:05:22.590 Well the United States is a really interesting place because it's kind of sandwiched between the 80 00:05:22.610 --> 00:05:26.630 tropics and the higher latitudes. And what that allows us to have is a lot of 81 00:05:26.650 --> 00:05:30.700 different weather patterns in different regions. Now what matters in this 82 00:05:30.720 --> 00:05:34.770 region is that you see these storm systems moving from west to east 83 00:05:34.790 --> 00:05:38.790 across the country and that can dump a lot of rainfall in the midwest, but we've 84 00:05:38.810 --> 00:05:42.790 observed out west in California is a prolonged absense 85 00:05:42.810 --> 00:05:46.860 of rain actually causing lots of draught. And so what's important is that 86 00:05:46.880 --> 00:05:50.870 we can get this global picture, even this U.S. picture, to understand 87 00:05:50.890 --> 00:05:54.930 where we're getting more and less rainfall and how that's impacting our society. 88 00:05:54.950 --> 00:05:58.950 89 00:05:58.970 --> 00:06:02.970 90 00:06:02.990 --> 00:06:07.010 That really gets at the 91 00:06:07.030 --> 00:06:11.230 notion of climate zones. If you have precipitation 92 00:06:11.250 --> 00:06:15.280 which is very steady and dependable, then the vegetation 93 00:06:15.300 --> 00:06:19.330 will grow that depends on having lots of steady vegetation. 94 00:06:19.350 --> 00:06:23.390 Steady precipitation. On the other hand 95 00:06:23.410 --> 00:06:27.410 if precipitation very intermitent, for example in the west coast. 96 00:06:27.430 --> 00:06:31.470 Particularly in the southern California. 97 00:06:31.490 --> 00:06:34.980 they have a so-called Mediterrean climate. It's very dry in the summertime 98 00:06:35.000 --> 00:06:39.950 and it's supposed to rain in the wintertime, but of course the last few years that hasn't happened. 99 00:06:39.970 --> 00:06:42.950 but, having that very intermittent precipitation 100 00:06:42.970 --> 00:06:47.020 introduces really fundamental changes in the kind of vegetation 101 00:06:47.040 --> 00:06:51.110 that's easy to grow there. 102 00:06:51.130 --> 00:06:56.150 103 00:06:56.170 --> 00:07:00.180 Well as you might imagine 104 00:07:00.200 --> 00:07:04.240 you can see from your local ground radars 105 00:07:04.260 --> 00:07:08.260 localized rain maps provided by the TV channels 106 00:07:08.280 --> 00:07:12.290 You can also see from satellite imagery white cloud tops taken 107 00:07:12.310 --> 00:07:16.340 at the tops of the clouds. So this new imagery allows us to provide 108 00:07:16.360 --> 00:07:20.370 uniform precipitation estimates using a constellation 109 00:07:20.390 --> 00:07:24.400 of satellites put all together. So you can 110 00:07:24.420 --> 00:07:28.500 see all the way down to the Earth's surface, the rain falling there impacting 111 00:07:28.520 --> 00:07:32.520 science and society. 112 00:07:32.540 --> 00:07:36.540 113 00:07:36.560 --> 00:07:40.560 114 00:07:40.580 --> 00:07:44.590 GPM is able to see the type of precipiation under the clouds 115 00:07:44.610 --> 00:07:48.630 because we are able to use the radar onboard. It's a new 116 00:07:48.650 --> 00:07:52.730 technology that allows you to see layer by layer within the clouds 117 00:07:52.750 --> 00:07:56.770 and within the precipitation. And so it provides something like a 118 00:07:56.790 --> 00:08:00.810 CT-scan that a doctor might use. And every 250 meters 119 00:08:00.830 --> 00:08:05.450 we see the structure of precipitation within the clouds with this radar 120 00:08:05.470 --> 00:08:11.060 instrument provided by the Japanese. 121 00:08:11.080 --> 00:08:17.980 122 00:08:18.000 --> 00:08:23.200 Absolutely. The annual pattern is referred to as a seasonal cycle so 123 00:08:23.220 --> 00:08:27.220 you certainly know in the United States it's cold in the winter 124 00:08:27.240 --> 00:08:31.270 warm in the summer. But in addition there are precipitation patterns that go along with 125 00:08:31.290 --> 00:08:34.960 that. That's true around the entire world. And of course in the southern hemisphere 126 00:08:34.980 --> 00:08:39.760 the seasons are reversed. Our summer is their winter and vice versa. 127 00:08:39.780 --> 00:08:44.140 In the tropics it's not really warm and cold is just wet and dry. 128 00:08:44.160 --> 00:08:48.860 There's lots of places where it's wet part of the year and then dry part of the year. 129 00:08:48.880 --> 00:08:51.790 And so these patterns repeat every year 130 00:08:51.810 --> 00:08:56.050 and then there are other interesting variations that actually go from.. between years 131 00:08:56.070 --> 00:09:01.970 So there is more than just the annual cycle 132 00:09:01.990 --> 00:09:05.990 133 00:09:06.010 --> 00:09:10.000 134 00:09:10.020 --> 00:09:14.050 So the patterns change most notably 135 00:09:14.070 --> 00:09:18.110 in the tropical regions because this is where the year to year 136 00:09:18.130 --> 00:09:22.140 fluxuations are the largest. So you have perhaps heard of El Nino 137 00:09:22.160 --> 00:09:26.190 and La Nina which originate in the Pacific Ocean. 138 00:09:26.210 --> 00:09:30.260 but extend well beyond that. In El Nino you 139 00:09:30.280 --> 00:09:34.310 have a massive amount of precipitation which is in the eastern Pacific Ocean 140 00:09:34.330 --> 00:09:38.360 and in La Nina you get a sort of reinforcement of the usual pattern where 141 00:09:38.380 --> 00:09:42.380 the equator doesn't have precipitation 142 00:09:42.400 --> 00:09:46.410 in the eastern Pacific Ocean. There are other patterns which 143 00:09:46.430 --> 00:09:50.460 we're less familiar with. There's something called the north Atlantic 144 00:09:50.480 --> 00:09:54.470 oscillation, the Antarctic oscillation. These are sort of technical 145 00:09:54.490 --> 00:09:58.510 sounding. But all it means is there's the repeating patterns that are 146 00:09:58.530 --> 00:10:02.560 maybe seasonal in length. In addition there are longer 147 00:10:02.580 --> 00:10:06.570 Patterns, the most notable of which is the Pacific decade of oscillation 148 00:10:06.590 --> 00:10:10.600 that's a really big sounding word, but all it means is it takes about a 149 00:10:10.620 --> 00:10:14.660 decade or 10 years for this pattern to work itself through. 150 00:10:14.680 --> 00:10:18.670 The implication of that of course is you need say 20 years of data in order to 151 00:10:18.690 --> 00:10:22.710 reliably detect the Pacific decade of oscillation. 152 00:10:22.730 --> 00:10:26.730 So there's a lot of really interesting patterns to study. 153 00:10:26.750 --> 00:10:30.750 154 00:10:30.770 --> 00:10:35.900 155 00:10:35.920 --> 00:10:38.830 Well I think debunked is maybe not 156 00:10:38.850 --> 00:10:42.870 quite the term, but what we've got is a search to 157 00:10:42.890 --> 00:10:46.980 understand better what's going on. And so for example we 158 00:10:47.000 --> 00:10:50.980 always have known that there is snow at the top of hurricanes, 159 00:10:51.000 --> 00:10:54.480 but when we get these data which are for the first time are really working 160 00:10:54.500 --> 00:10:59.210 systematically to visualize snow, when you look at a hurricane, for example Hurricane 161 00:10:59.230 --> 00:11:03.020 Arthur, you see snow at the top. So the warm 162 00:11:03.040 --> 00:11:07.070 colors toward the surface are rain and the cool blue colors 163 00:11:07.090 --> 00:11:10.780 at the top are snow. Who knew all over the tropics it's 164 00:11:10.800 --> 00:11:15.480 snowing just four miles up. Another important factor 165 00:11:15.500 --> 00:11:18.980 that we haven't really understood is the precipitation 166 00:11:19.000 --> 00:11:23.230 in the Southern Ocean. There's very little land there. It's a very rough 167 00:11:23.250 --> 00:11:27.250 weather and people don't go there unless they have to. And so this 168 00:11:27.270 --> 00:11:31.290 satellite system allows us to systematically view 169 00:11:31.310 --> 00:11:35.340 the Southern Ocean in a way that we haven't before and I'm really hopeful that 170 00:11:35.360 --> 00:11:39.696 we will now see much more quantitative, accurate results there.