WEBVTT FILE 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]