1 00:00:12,070 --> 00:00:07,670 a monsoon is a 2 00:00:17,430 --> 00:00:15,270 it is classified in terms of a 3 00:00:21,910 --> 00:00:17,440 prevailing strong winds 4 00:00:23,029 --> 00:00:21,920 that reverse distinctly as the season 5 00:00:26,310 --> 00:00:23,039 and also 6 00:00:28,230 --> 00:00:26,320 it is described by a very distinct wet 7 00:00:31,109 --> 00:00:28,240 and dry season 8 00:00:35,270 --> 00:00:31,119 the rainfall that fall within that wet 9 00:00:37,430 --> 00:00:35,280 season should should be more than 60 10 00:00:39,350 --> 00:00:37,440 of the entire year 11 00:00:40,950 --> 00:00:39,360 the fundamental drive for the monsoon 12 00:00:42,630 --> 00:00:40,960 both in india and other parts of the 13 00:00:44,549 --> 00:00:42,640 world is that there's a large area of 14 00:00:46,630 --> 00:00:44,559 land which gets warm compared to their 15 00:00:48,869 --> 00:00:46,640 surrounding ocean and that surrounding 16 00:00:51,029 --> 00:00:48,879 ocean provides the moisture which is 17 00:00:53,990 --> 00:00:51,039 then driving the precipitation that 18 00:00:56,470 --> 00:00:54,000 constitutes what we think of as monsoon 19 00:00:58,549 --> 00:00:56,480 if you simply look at asian monsoon you 20 00:01:01,029 --> 00:00:58,559 can estimate and various estimate more 21 00:01:03,430 --> 00:01:01,039 than 60 percent of the world population 22 00:01:06,789 --> 00:01:03,440 live in right in that area 23 00:01:09,190 --> 00:01:06,799 and the monsoon the water provided fresh 24 00:01:11,190 --> 00:01:09,200 water supply for this population not 25 00:01:13,510 --> 00:01:11,200 just for the daily life for agriculture 26 00:01:16,550 --> 00:01:13,520 for the for the industry and so the 27 00:01:19,109 --> 00:01:16,560 entire region the people's livelihood 28 00:01:22,469 --> 00:01:19,119 depend on the very delicate balance of 29 00:01:24,390 --> 00:01:22,479 the water balance in that region 30 00:01:26,950 --> 00:01:24,400 gpm gives us a chance to look at 31 00:01:28,870 --> 00:01:26,960 precipitation around the world and so in 32 00:01:30,950 --> 00:01:28,880 addition to the hurricanes and typhoons 33 00:01:32,870 --> 00:01:30,960 we're also looking at the monsoons 34 00:01:34,950 --> 00:01:32,880 because those storm systems are very 35 00:01:35,910 --> 00:01:34,960 important for driving floods 36 00:01:37,990 --> 00:01:35,920 and 37 00:01:39,350 --> 00:01:38,000 the advancements in gpm will allow us to 38 00:01:41,109 --> 00:01:39,360 do a better job of providing 39 00:01:43,190 --> 00:01:41,119 precipitation information so they can 40 00:01:45,190 --> 00:01:43,200 make better forecasts of the floods 41 00:01:48,069 --> 00:01:45,200 monsoon is not just simply a local 42 00:01:50,710 --> 00:01:48,079 problem a curiosity it actually has a 43 00:01:52,789 --> 00:01:50,720 huge amount of societal 44 00:01:54,550 --> 00:01:52,799 impact in terms of how it changes in 45 00:01:57,190 --> 00:01:54,560 that region the economy in that region 46 00:01:58,709 --> 00:01:57,200 can affect the entire world as well as 47 00:01:59,990 --> 00:01:58,719 many many things that happen in that 48 00:02:03,670 --> 00:02:00,000 region 49 00:02:06,709 --> 00:02:03,680 gpm has the most advanced duo frequency 50 00:02:09,109 --> 00:02:06,719 radar that actually measures the 51 00:02:11,029 --> 00:02:09,119 vertical structure of the ring for 52 00:02:13,190 --> 00:02:11,039 itself and that's very important 53 00:02:16,390 --> 00:02:13,200 the dpr gives us an unprecedented 54 00:02:17,910 --> 00:02:16,400 capability of teasing out relative sizes 55 00:02:19,910 --> 00:02:17,920 of particles and this is really 56 00:02:22,710 --> 00:02:19,920 important for understanding how the 57 00:02:25,430 --> 00:02:22,720 microphysics the the rain process works 58 00:02:27,350 --> 00:02:25,440 and the snow process and also how those 59 00:02:29,589 --> 00:02:27,360 can then be represented in numerical 60 00:02:31,830 --> 00:02:29,599 models that are critical for forecasting 61 00:02:34,790 --> 00:02:31,840 future events to study the monsoon one 62 00:02:36,470 --> 00:02:34,800 thing we didn't know is to note what we 63 00:02:38,150 --> 00:02:36,480 call the predictability in the monsoon 64 00:02:40,070 --> 00:02:38,160 how well can we predict the monsoon at 65 00:02:42,550 --> 00:02:40,080 that time and in order to do the 66 00:02:44,869 --> 00:02:42,560 prediction we need to have to know the 67 00:02:47,670 --> 00:02:44,879 variability very well this ranges from 68 00:02:50,229 --> 00:02:47,680 daily to weekly seasonal and then to 69 00:02:52,790 --> 00:02:50,239 what we call decadal variability the 70 00:02:54,710 --> 00:02:52,800 monsoon was first named in india 71 00:02:56,150 --> 00:02:54,720 but it turns out that the same driving 72 00:02:58,630 --> 00:02:56,160 force happens in other parts of the 73 00:03:01,270 --> 00:02:58,640 world and so for example in the northern 74 00:03:03,589 --> 00:03:01,280 hemisphere summer you have monsoon in 75 00:03:06,550 --> 00:03:03,599 west africa you have the monsoon in 76 00:03:08,309 --> 00:03:06,560 southwestern north america and then in 77 00:03:10,949 --> 00:03:08,319 our winter the southern hemisphere 78 00:03:13,110 --> 00:03:10,959 summer there's a monsoon that happens 79 00:03:15,030 --> 00:03:13,120 across northern australia 80 00:03:17,589 --> 00:03:15,040 the great thing about gpm is it allows 81 00:03:19,190 --> 00:03:17,599 you to see the orange systems as a whole 82 00:03:20,710 --> 00:03:19,200 you get to see them over the ocean and 83 00:03:22,869 --> 00:03:20,720 over the land you can see what the 84 00:03:24,869 --> 00:03:22,879 transitions are and so even before it 85 00:03:27,110 --> 00:03:24,879 gets to land where we have surface 86 00:03:29,670 --> 00:03:27,120 observations we can tell what's going to 87 00:03:31,270 --> 00:03:29,680 come in we can see what's been happening 88 00:03:32,789 --> 00:03:31,280 and of course scientifically that also 89 00:03:34,630 --> 00:03:32,799 allows us to understand the complete