1 00:00:12,400 --> 00:00:04,040 [Music] 2 00:00:12,400 --> 00:00:16,440 NASA's Operation IceBridge 3 00:00:16,440 --> 00:00:20,550 Mission the largest airborne survey of adverse polar ice every flown 4 00:00:20,550 --> 00:00:24,650 kicks off it's second year with the arrival of two NASA aircraft next week in Greenland. 5 00:00:24,650 --> 00:00:28,680 The team will spend 200 hours gathering data using a suite 6 00:00:28,680 --> 00:00:32,720 of instruments that peer below some of the regions critical glaciers 7 00:00:36,930 --> 00:00:32,750 IceBridge is aptly named because it will bridge the data gap between 8 00:00:36,930 --> 00:00:41,080 the loss of NASA's Ice Cloud and Land elevation satellite, or ICESat 9 00:00:41,080 --> 00:00:45,120 and the launch of ICESat 2 planned for 2015. 10 00:00:45,120 --> 00:00:49,290 [John Sonntag] I think its probably safe to say if it weren't for Operation IceBridge 11 00:00:49,290 --> 00:00:53,480 or the similar efforts that the global science community would lose a lot of its knowledge 12 00:00:53,480 --> 00:00:57,530 of what's going on with Greenland and Antarctica as a whole. 13 00:00:57,530 --> 00:01:01,540 [Narrator] 200 hours in the air, require a lot of work on the ground 14 00:01:01,540 --> 00:01:05,660 engineers have been outfitting NASA's DC8 and PB3 aircraft with an array of 15 00:01:05,660 --> 00:01:09,830 science instruments. IceBridge planes 16 00:01:09,830 --> 00:01:14,010 resurvey previous ICESat tracks to get a sense of how arctic ice is changing. 17 00:01:14,010 --> 00:01:18,050 [John Sonntag] I think the last thing that NASA would like to see is 18 00:01:18,050 --> 00:01:22,230 to take a snap shot of the ice at the end of ICESat 1 19 00:01:22,230 --> 00:01:26,250 operational period. Get another snap shot at the beginning of ICESat 20 00:01:26,250 --> 00:01:30,320 2 and have no idea what happen in between. That is essentially what IceBridge is about 21 00:01:30,320 --> 00:01:34,510 is filling in that gap knowledge. [Bryan Blair] If you want to look at 22 00:01:34,510 --> 00:01:38,680 areas that are very dynamic like a glacial region 23 00:01:38,680 --> 00:01:42,770 its like a lot of ice moving through and there is a lot of vertical changes, we can map that entire 24 00:01:42,770 --> 00:01:46,830 area and capture the full spacial variably of 25 00:01:46,830 --> 00:01:50,850 that change. Which is a really good indication of what's the mechanics of 26 00:01:50,850 --> 00:01:54,870 how that change is happening. [John Sonntag] Greenland because of it's 27 00:01:54,870 --> 00:01:58,960 presence and Antarctica all the ice mass act as a buffer and climate 28 00:01:58,960 --> 00:02:03,130 and so if they were to start to melt, which many people 29 00:02:03,130 --> 00:02:07,310 believe that they are. Then the eventual affect will be a 30 00:02:07,310 --> 00:02:11,340 warmer climate over all. [Narrator] Annual spring missions over the 31 00:02:11,340 --> 00:02:15,530 arctic and fall missions over Antarctica will allow scientists to track changes 32 00:02:15,530 --> 00:02:19,550 in polar ice thickness and extent, so we have a better picture of ice dynamics. 33 00:02:19,550 --> 00:02:23,620 and future sea level rise.