WEBVTT FILE 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]