1 00:00:00,020 --> 00:00:04,090 [aircraft sound] 2 00:00:04,110 --> 00:00:08,140 We are currently on our mission down to Pine Island Glacier in west Antarctica 3 00:00:08,160 --> 00:00:12,190 and we will be flying about a 3 hour survey there over the glacier. 4 00:00:12,210 --> 00:00:16,250 Pine Island Glacier losing ice very quickly 5 00:00:16,270 --> 00:00:20,290 about 6 meters per year and today we will go back and re-fly 6 00:00:20,310 --> 00:00:24,380 the same mission that we have flown two years earlier in 2009. 7 00:00:24,400 --> 00:00:28,440 And we can compare the data that we collect today to our previous data 8 00:00:28,460 --> 00:00:32,480 and also to the data of the ICESat satellite that has collected 9 00:00:32,500 --> 00:00:36,530 surface elevation measurements there over many years. And this will tell us 10 00:00:36,550 --> 00:00:40,620 how much ice is being lost in west Antarctica 11 00:00:40,640 --> 00:00:44,700 and contributes to sea level rise. 12 00:00:44,720 --> 00:00:48,760 Two weeks ago we had another mission over Pine Island Glacier 13 00:00:48,780 --> 00:00:52,780 and when looking out of the window of the aircraft we noticed 14 00:00:52,800 --> 00:00:56,820 a fairly large crack in the ice shelf. 15 00:00:56,840 --> 00:01:00,910 And I talked back to colleagues in the U.S. that downloaded satellite images 16 00:01:00,930 --> 00:01:04,960 and they reported that this crack has formed in sometime between 17 00:01:04,980 --> 00:01:08,980 end of September or early October. 18 00:01:09,000 --> 00:01:13,020 These things happen on a semi-regular basis in both the Arctic and the Antarctic, 19 00:01:13,040 --> 00:01:17,140 but it’s still a fairly large event. 20 00:01:17,160 --> 00:01:21,150 So we wanted to make sure we captured as much of that process as we could. 21 00:01:21,170 --> 00:01:25,170 So today was our first trip to be back in the area and what we do is we modified the existing flight plan 22 00:01:25,190 --> 00:01:29,280 to add another half hour to the flight in order to catch a flight along the 23 00:01:29,300 --> 00:01:33,350 direction of the rift, in order to get mainly a lidar and photographic map of 24 00:01:33,370 --> 00:01:37,410 the shape, depth of the rift, and the width of it -- see how it's developing over time. 25 00:01:37,430 --> 00:01:41,440 At the moment the crack is about 80 meters wide. 26 00:01:41,460 --> 00:01:45,490 If it continues to propagate, it's about an iceberg that ice the area of 800 square kilometers 27 00:01:45,510 --> 00:01:49,520 that eventually will break off from the 28 00:01:49,540 --> 00:01:53,590 Pine Island Glacier. 29 00:01:53,610 --> 00:01:57,720 Now if we're lucky, we may get another chance to come back to this area later, if weather and 30 00:01:57,740 --> 00:02:01,890 timing permits, to do what we just did today to see how the rift has further developed as time goes on. 31 00:02:01,910 --> 00:02:05,930 A lot of times when you're in science you 32 00:02:05,950 --> 00:02:10,060 don't get a chance to catch the big stories as they happen because you're 33 00:02:10,080 --> 00:02:14,130 not there at the right time, but this time we were.