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.