1 00:00:00,010 --> 00:00:04,080 [wind noises] 2 00:00:04,100 --> 00:00:08,130 [music] 3 00:00:08,150 --> 00:00:12,150 Hello. My name’s María José Viñas and I am a science writer for NASA. 4 00:00:12,170 --> 00:00:16,270 I’m here in Greenland, in a town named Kangerlussuaq, 5 00:00:16,290 --> 00:00:20,340 accompanying a mission called IceBridge, or Puente de Hielo. 6 00:00:20,360 --> 00:00:24,370 This is the plane we use for our mission, 7 00:00:24,390 --> 00:00:28,480 a P-3B, which used to be a military plane that was readapted to be used for scientific missions. 8 00:00:28,500 --> 00:00:32,580 It’s equipped with a series of instruments that I will tell you about later. 9 00:00:32,600 --> 00:00:36,650 [music, aircraft noise] 10 00:00:36,670 --> 00:00:40,720 With IceBridge we fly this airplane quite close to the ground, 11 00:00:40,740 --> 00:00:44,770 at about 450 meters above the surface, and using a series of lasers and radars 12 00:00:44,790 --> 00:00:48,950 to observe how the ice sheet evolves from year to year. 13 00:00:48,970 --> 00:00:53,060 [music, aircraft noise] 14 00:00:53,080 --> 00:00:57,090 We do this twice a year: from October to December we go to Antarctica 15 00:00:57,110 --> 00:01:01,160 and from March til May we’re here in Greenland, measuring the Arctic ice sheet. 16 00:01:01,180 --> 00:01:05,350 For example, this morning we’ve flown over Jakobshavn Glacier, 17 00:01:05,370 --> 00:01:09,450 one of the fastest melting glaciers in the world 18 00:01:09,470 --> 00:01:13,480 and we’ve measured how high it is this year, and we’ll compare this with data 19 00:01:13,500 --> 00:01:17,610 from previous years, to find out how much [of the glacier] has disappeared in one year. 20 00:01:17,630 --> 00:01:21,660 The P-3B carries a laser 21 00:01:21,680 --> 00:01:25,680 and four types of radar. The laser emits a pulse of light that bounces off the ice surface: 22 00:01:25,700 --> 00:01:29,780 the time that it takes for the light to return to the receivers installed 23 00:01:29,800 --> 00:01:33,830 in the body of the plane is indicative of the height of the ice sheet. 24 00:01:33,850 --> 00:01:37,880 The radars work in a similar way, but they use electromagnetic energy, 25 00:01:37,900 --> 00:01:42,030 which is able to penetrate the ice sheet and obtain information about its depth and structure. 26 00:01:42,050 --> 00:01:46,050 Two other instruments onboard the aircraft, called the gravetometer and magnetometer, 27 00:01:46,070 --> 00:01:50,110 analyze the geologic composition of the ground. 28 00:01:50,130 --> 00:01:54,200 Scientists study the data obtained during each IceBridge campaign 29 00:01:54,220 --> 00:01:58,270 and compare it to data from previous years, to calculate how 30 00:01:58,290 --> 00:02:02,380 the ice sheet changes from year to year. 31 00:02:02,400 --> 00:02:06,440 Here we are at the Russell Glacier, at the feet of Greenland’s ice sheet 32 00:02:06,460 --> 00:02:10,480 extending kilometers and kilometers into the interior of Greenland. 33 00:02:10,500 --> 00:02:14,590 And when you see this immensity is a bit hard to imagine 34 00:02:14,610 --> 00:02:18,670 disappear one day but that is what is happening right now, it's melting