1 00:00:08,360 --> 00:00:04,180 [music] 2 00:00:08,380 --> 00:00:12,540 Greetings from Punta Arenas, our base of operations for the Antarctic campaign of NASA’s Operation IceBridge. 3 00:00:12,560 --> 00:00:16,730 Punta Arenas is the capital of Chile’s southern region 4 00:00:16,750 --> 00:00:20,910 and one of the main jumping off points for Antarctica. 5 00:00:20,930 --> 00:00:25,110 Behind me there’s a replica of the lifeboat James Caird, 6 00:00:25,130 --> 00:00:29,300 which the Antarctic explorer Ernest Shackelton used to escape Elephant Island 7 00:00:29,320 --> 00:00:33,470 after his ship, Endurance, sank in the Weddell Sea. 8 00:00:33,490 --> 00:00:37,590 The spirit of this explorer is an inspiration to IceBridge, which is dedicated 9 00:00:37,610 --> 00:00:41,690 to exploring remote areas of Antarctica to observe changes to the ice sheet 10 00:00:41,710 --> 00:00:45,750 covering the continent and the sea ice surrounding it. 11 00:00:45,770 --> 00:00:49,810 It takes between three and four hours to reach Antarctica from southern Chile. 12 00:00:49,830 --> 00:00:53,870 Since flights are longer than those of the Arctic campaign, we use 13 00:00:53,890 --> 00:00:57,910 another type of plane, a DC-8, which can carry larger quantities 14 00:00:57,930 --> 00:01:01,950 of fuel and thus lets us reach very remote areas of the frozen continent. 15 00:01:01,970 --> 00:01:06,130 This is the fourth year that IceBridge has explored Antarctica, since the 16 00:01:06,150 --> 00:01:10,320 mission began in 2009. In total, there are sixteen missions planned for 17 00:01:10,340 --> 00:01:14,500 for this campaign: twelve will study land ice and the remaining four 18 00:01:14,520 --> 00:01:18,670 will observe the ice floating on the seas of Weddell, Bellingshausen and Amundsen, in the 19 00:01:18,690 --> 00:01:22,850 the western sector of the continent. IceBridge uses several instruments to study 20 00:01:22,870 --> 00:01:27,010 sea ice. On one hand, a laser measures the freeboard, 21 00:01:27,030 --> 00:01:31,190 or the height of the ice floe above the water surface. On the other hand, one of the radars 22 00:01:31,210 --> 00:01:35,350 radars onboard the DC-8, assisted by the laser, measures the snow layer 23 00:01:35,370 --> 00:01:39,410 accumulated over sea ice. The combination of the two 24 00:01:39,430 --> 00:01:43,480 data sets allows scientists to calculate the total thickness of sea ice 25 00:01:43,500 --> 00:01:47,590 including the fraction that is under water. Finally, a high-definition 26 00:01:47,610 --> 00:01:51,670 camera system takes images that will help researchers locate leads between ice floes. 27 00:01:51,690 --> 00:01:55,720 The areas of land ice of greatest interest to IceBridge 28 00:01:55,740 --> 00:01:59,750 are located in the west coast of Antarctica, where 29 00:01:59,770 --> 00:02:03,930 the largest changes are taking place. One of the glaciers that is most quickly 30 00:02:03,950 --> 00:02:08,120 losing ice to the sea is Pine Island Glacier, southwest of the Antarctica Peninsula. 31 00:02:08,140 --> 00:02:12,300 During the 2011 campaign, IceBridge discovered 32 00:02:12,320 --> 00:02:16,390 a huge crack that crossed Pine Island’s ice shelf 33 00:02:16,410 --> 00:02:20,580 almost entirely. It's thought that when it breaks, 34 00:02:20,600 --> 00:02:24,760 it will create an enormous iceberg the size of Manhattan. 35 00:02:24,780 --> 00:02:28,940 But when NASA’s DC-8 visited Pine Island Glacier again in 2012, 36 00:02:28,960 --> 00:02:33,100 , the crack was still there, only wider and with a secondary crack. 37 00:02:33,120 --> 00:02:37,240 And so the iceberg remains for now. 38 00:02:37,260 --> 00:02:41,370 Meanwhile, the data collected by IceBridge instruments 39 00:02:41,390 --> 00:02:45,550 over Pine Island and the neighboring Thwaites Glacier 40 00:02:45,570 --> 00:02:49,670 will allow researchers to revisit previous years’ measurements and determine 41 00:02:49,690 --> 00:02:53,760 how the ice flow is evolving in that corner of Antarctica.