WEBVTT FILE 1 00:00:00.010 --> 00:00:04.040 2 00:00:04.059 --> 00:00:08.079 Gail: Actually the snow right now is not abnormal right now. What we're seeing 3 00:00:08.100 --> 00:00:12.110 over the past couple of years is that snow can vary from month to month 4 00:00:12.130 --> 00:00:16.130 and over the past few winters, yeah, we've seen a lot of snow, but this year, there's not much 5 00:00:16.149 --> 00:00:20.150 snow, but it's not by far the least amount of snow that we've had. 6 00:00:20.170 --> 00:00:24.160 2006 had less snow. and as we would recall in 2010 we had 7 00:00:24.180 --> 00:00:28.180 quite a bit of snow. So it's really not abnormal; it's just the global cycle working 8 00:00:28.200 --> 00:00:32.200 together. 9 00:00:32.220 --> 00:00:36.239 There's lots of impacts for not having enough snow. Snow is quite an 10 00:00:36.260 --> 00:00:40.290 important part of the water cycle. When snow falls it lands on snowpacks, and it's 11 00:00:40.310 --> 00:00:44.340 stays there. It's like a battery and it holds the energy of that snow 12 00:00:44.360 --> 00:00:48.370 it holds that water. So that when it melts out in the spring and the summer, we can use that 13 00:00:48.390 --> 00:00:52.410 for water resources. If we get less snow, that means that it melts earlier 14 00:00:52.430 --> 00:00:56.430 and also there's an issue with if it melts, 15 00:00:56.450 --> 00:01:00.450 it means that the Earth, which is typically reflective when there's snow cover; it's like a 16 00:01:00.470 --> 00:01:04.459 mirror, it allows it to absorb more heat. So we really want to have as much snow as 17 00:01:04.480 --> 00:01:08.470 we can for our normal cycles. 18 00:01:08.490 --> 00:01:12.530 Yeah, there were a couple factors 19 00:01:12.550 --> 00:01:16.570 that NASA researchers have recently uncovered. One of th 20 00:01:16.590 --> 00:01:20.620 big things for the Snowmageddon in 2010 is that we were in an El Nino 21 00:01:20.640 --> 00:01:24.650 year, and what that means is that there's a lot of moisture from the 22 00:01:24.670 --> 00:01:28.690 Pacific Ocean was uplifted and brought over the U.S. And what happened 23 00:01:28.710 --> 00:01:32.710 there, then it's deposited in the southeast U.S. 24 00:01:32.730 --> 00:01:36.720 came up the east coast. And then what we had was another factor, which was 25 00:01:36.740 --> 00:01:40.729 called the North Atlantic Oscillation, and in 2010 it was persistently 26 00:01:40.750 --> 00:01:44.740 negative. And really what that means is that there was a high pressure system over the polar 27 00:01:44.760 --> 00:01:48.790 regions that was pushing cold air down. So the interacting moisture for 28 00:01:48.810 --> 00:01:52.830 the Pacific Ocean with the cold air from the Arctic, what happens then is 29 00:01:52.850 --> 00:01:56.880 we get snow, and we got a lot of snow in 2010. 30 00:01:56.900 --> 00:02:00.910 There's many reasons to study 31 00:02:00.930 --> 00:02:04.940 snow from space. Sure, you can go in your backyard or use your radar 32 00:02:04.960 --> 00:02:08.959 to measure it from space. But over the oceans there's 33 00:02:08.979 --> 00:02:12.980 no way to measure the snow. When you measure snow from space you can get uniform 34 00:02:13.000 --> 00:02:16.990 measurements that can be applied globally and also can be used 35 00:02:17.010 --> 00:02:21.000 in models for better forecasting for weather and for better forecasting 36 00:02:21.020 --> 00:02:25.050 of the climate change and how we are going to predict climate change. 37 00:02:25.070 --> 00:02:29.090 38 00:02:29.110 --> 00:02:33.120 NASA is doing some great things right now to understand winter storm mechanics. 39 00:02:33.140 --> 00:02:37.149 We have a field campaign going on right now which is in the January 40 00:02:37.170 --> 00:02:41.179 time period of 2012. We've got an aircraft called the DC-8, which many of you 41 00:02:41.200 --> 00:02:45.209 might have flown on, and I was actually on last week. And this aircraft is flying 42 00:02:45.230 --> 00:02:49.220 over the tops of the snow clouds over southern Ontario. And with it we're also 43 00:02:49.240 --> 00:02:53.240 measuring some other information with other spiralling aircraft, and we've 44 00:02:53.260 --> 00:02:57.239 put all this information together to get a three-dimensional structure of the snow. 45 00:02:57.260 --> 00:03:01.290 We're going to use that for Global Precipitation Measurement, which is a satellite 46 00:03:01.310 --> 00:03:05.330 that's going to be launched in 2014. And this satellite is going to provide us everything 47 00:03:05.350 --> 00:03:09.370 from the heavy tropical rain you might see in hurricanes all the way through the snow. 48 00:03:09.390 --> 00:03:13.399 And the information we're getting right now is going to help improve those models 49 00:03:13.420 --> 00:03:17.410 and to help improve our forecasting in the future. 50 00:03:17.430 --> 00:03:21.440 51 00:03:21.460 --> 00:03:25.450 [beep, beep...] 52 00:03:25.470 --> 00:03:29.460 53 00:03:29.480 --> 00:03:30.190