1 00:00:00,020 --> 00:00:04,030 [NATURAL SOUND] 2 00:00:04,050 --> 00:00:08,100 Houze: The weather has been extremely robust 3 00:00:08,120 --> 00:00:12,240 and informative. We've had good 4 00:00:12,260 --> 00:00:16,370 forecasting of the weather so we can plan our campaign. 5 00:00:16,390 --> 00:00:20,570 Petersen: I'm fairly confident in saying that the OLYMPEX field campaign is one of the best that 6 00:00:20,590 --> 00:00:24,650 we've done yet, bar none. It was a very nice way to finish off our major ground validation 7 00:00:24,670 --> 00:00:28,770 field campaigns for GPM and that we really just nailed it with OLYMPEX. 8 00:00:28,790 --> 00:00:32,970 Houze: As you know the Olympic Mountains 9 00:00:32,990 --> 00:00:37,080 are the really the only temperate rainforest area in 10 00:00:37,100 --> 00:00:41,240 the Northern Hemisphere, and we get lots, 11 00:00:41,260 --> 00:00:45,400 lots of storms every winter, and I think the excitement is that we 12 00:00:45,420 --> 00:00:49,620 have gotten such a good sequence of weather patterns with 13 00:00:49,640 --> 00:00:53,800 very heavy rain storms. We've had several flooding events, 14 00:00:53,820 --> 00:00:57,970 we have one radar which is perched by the side of the Quinault 15 00:00:57,990 --> 00:01:02,150 River. In fact it became so high at one point that they had to literally 16 00:01:02,170 --> 00:01:06,290 raise the radar and its truck that it sits on up 17 00:01:06,310 --> 00:01:10,390 several feet and the radar operators ended up having to 18 00:01:10,410 --> 00:01:14,520 kayak to the radar. Petersen: The storm that I really got excited 19 00:01:14,540 --> 00:01:18,590 about was a storm where we did our very first-ever triple-aircraft stacked sampling underneath 20 00:01:18,610 --> 00:01:22,640 the GPM Core satellite as it flew over the top 21 00:01:22,660 --> 00:01:26,820 while at the same time we were looking up at the precipitation from below the base of the 22 00:01:26,840 --> 00:01:30,900 mountains with three different radars. The system itself was a very 23 00:01:30,920 --> 00:01:35,060 complex precipitation system. The flow was coming in off the ocean and impinging on the mountains 24 00:01:35,080 --> 00:01:39,170 and then the precipitation got very deep over the mountains. Whereas 25 00:01:39,190 --> 00:01:43,380 it was much shallower over the ocean, and so we were able to see this ice process 26 00:01:43,400 --> 00:01:47,500 over the mountains that wasn't quite as pronounced over the ocean so there's a big 27 00:01:47,520 --> 00:01:51,600 transition in how the precipitation and the rainfall was made between just those two areas over a 28 00:01:51,620 --> 00:01:55,770 short distance. The dataset that we've collected so far--there's no question-- 29 00:01:55,790 --> 00:01:59,860 it's going to really contribute to being able to understand both the precipitation 30 00:01:59,880 --> 00:02:04,060 processes that are occurring, but how we do a better job of measuring those processes from 31 00:02:04,080 --> 00:02:08,110 space. [MUSIC] 32 00:02:08,130 --> 00:02:11,245 [MUSIC]