1 00:00:00,020 --> 00:00:04,010 [guitar strumming] >>Singing: ICESat 2 00:00:04,030 --> 00:00:08,040 launched 11 years ago, measuring 3 00:00:08,060 --> 00:00:12,070 ice, glaciers and snow. Lasers 4 00:00:12,090 --> 00:00:16,090 housed in a device called "GLAS", observed the Earth 5 00:00:16,110 --> 00:00:20,110 and sent the data fast. Lasers bounced off the 6 00:00:20,130 --> 00:00:24,150 polar sector, mapping the Earth with a 7 00:00:24,170 --> 00:00:28,180 photon collector. Lasers captured both width 8 00:00:28,200 --> 00:00:32,210 and depth, so we can better study the polar 9 00:00:32,230 --> 00:00:36,240 breadth. Using our laser technology, 10 00:00:36,260 --> 00:00:40,260 results in 3D cartography. 11 00:00:40,280 --> 00:00:44,330 Using our laser technology, we can 12 00:00:44,350 --> 00:00:48,390 do accurate topography. 13 00:00:48,410 --> 00:00:52,460 >>Anna: As the global sea level continues to rise, it becomes more and more 14 00:00:52,480 --> 00:00:56,520 necessary to map how much land ice has melted. But 15 00:00:56,540 --> 00:01:00,580 how do we map such a big area with any accuracy? The answer 16 00:01:00,600 --> 00:01:04,650 is lasers. >>Geof: Photos show the changes 17 00:01:04,670 --> 00:01:08,720 in the surface area of ice, but don't show depth. Lasers can measure 18 00:01:08,740 --> 00:01:12,750 topography to within an inch. Because of that precision and speed, laser ranging instruments 19 00:01:12,770 --> 00:01:16,770 are in use to measure the surface topography of the ice and study how much ice has been 20 00:01:16,790 --> 00:01:20,810 lost. >>Anna: NASA measure two types of ice. Ice on land, 21 00:01:20,830 --> 00:01:24,830 and sea ice. Ice sheets and glaciers found on land, like 22 00:01:24,850 --> 00:01:28,860 Greenland and Antarctica, are formed as snow accumulates 23 00:01:28,880 --> 00:01:32,890 and is compacted into ice. Sea ice on the other hand, is frozen 24 00:01:32,910 --> 00:01:36,960 sea water found floating in the Arctic Ocean and offshore of Antarctica. 25 00:01:36,980 --> 00:01:41,040 >>Geof: IceBridge flights over the ocean near Greenland allow 26 00:01:41,060 --> 00:01:45,060 researchers to measure the height differences between open water and sea ice, 27 00:01:45,080 --> 00:01:49,170 which is key to determining the ice thickness. >>Anna: ICESat-2 will measure elevation 28 00:01:49,190 --> 00:01:53,210 across Earth's entire surface, including vegetation 29 00:01:53,230 --> 00:01:57,240 and oceans, but with a focus on change in the frozen areas of 30 00:01:57,260 --> 00:02:01,330 the planet where scientists have observed dramatic impacts on 31 00:02:01,350 --> 00:02:05,370 climate change. ICESat-2 will be launched in the near future. 32 00:02:05,390 --> 00:02:09,400 Until then, follow NASA's mapping missions. >>Singing: 2010 33 00:02:09,420 --> 00:02:13,460 was the end of the mission. IceBridge 34 00:02:13,480 --> 00:02:17,500 and LVIS flew into position. Crisscrossing 35 00:02:17,520 --> 00:02:21,530 grids across the ice, measuring once, 36 00:02:21,550 --> 00:02:25,560 measuring twice. ICESat-2 in the 37 00:02:25,580 --> 00:02:29,580 next few years, will launch to measure 38 00:02:29,600 --> 00:02:33,600 new frontiers. ICESat's laser 39 00:02:33,620 --> 00:02:37,610 technology, reveals our hidden 40 00:02:37,630 --> 00:02:41,620 geography. Using our laser technology, 41 00:02:41,640 --> 00:02:45,640 results in 3D cartography. 42 00:02:45,660 --> 00:02:49,690 Using our laser technology, 43 00:02:49,710 --> 00:02:53,760 we can do accurate topography. 44 00:02:53,780 --> 00:02:57,810 [guitar strumming] 45 00:02:57,830 --> 00:03:01,840 [guitar strumming] 46 00:03:01,860 --> 00:03:05,165 [final guitar strum]