WEBVTT FILE 1 00:00:00.030 --> 00:00:04.080 NASA is about to launch the most advanced laser instrument of its kind, 2 00:00:04.100 --> 00:00:08.110 the Ice, Cloud and land Elevation Satellite-2, or ICESat-2, 3 00:00:08.130 --> 00:00:12.130 will measure changes in glaciers, ice sheets and sea ice. So to prepare 4 00:00:12.150 --> 00:00:16.200 for launch, we're counting down ten quick facts about ICESat-2. 5 00:00:16.220 --> 00:00:20.220 Ten thousand. That's how many times the ICESat-2 laser will fire 6 00:00:20.240 --> 00:00:24.240 each second. More pulses mean more height data. The fast-firing 7 00:00:24.260 --> 00:00:28.290 laser will allow us to measure the average annual change in the vast ice sheets 8 00:00:28.310 --> 00:00:32.310 down to the width of a pencil. Nine years of data from Operation 9 00:00:32.330 --> 00:00:36.340 IceBridge will be added to ICESat-2's new data. The airborne mission 10 00:00:36.360 --> 00:00:40.370 bridged the gap between the original ICESat and ICEsat-2 with 11 00:00:40.390 --> 00:00:44.410 flights over the Arctic and Antarctica. Eight hundred picoseconds, 12 00:00:44.430 --> 00:00:48.450 less than one-billionth of a second. That's the precision at which individual 13 00:00:48.470 --> 00:00:52.500 laser photons will be timed as they complete their roundtrip journey from 14 00:00:52.520 --> 00:00:56.560 the satellite to the Earth and back. Seven kilometers per second is 15 00:00:56.580 --> 00:01:00.620 how fast ICESat-2 will zoom above the planet. It'll complete an orbit 16 00:01:00.640 --> 00:01:04.670 around Earth in 90 minutes. The orbits will converge around the poles, focusing the data 17 00:01:04.690 --> 00:01:08.760 in the regions with the most expected change. Six laser beams 18 00:01:08.780 --> 00:01:12.820 split from one on board ICESat-2. That's six times the beams 19 00:01:12.840 --> 00:01:16.880 of the original ICESat. More beams will cover more ground--or ice--and allow 20 00:01:16.900 --> 00:01:20.980 scientists to assess the slope of the surface they're measuring. 21 00:01:21.000 --> 00:01:25.090 Five hundred and thirty-two nanometers, the wavelength of the bright green laser. 22 00:01:25.110 --> 00:01:29.130 When these laser photons return to the satellite, filters block any light that's not exactly 23 00:01:29.150 --> 00:01:33.160 at this wavelength, keeping the amount of data noise down. 24 00:01:33.180 --> 00:01:37.190 Four times a year, every 91 days, ICESat-2 will measure the same ground 25 00:01:37.210 --> 00:01:41.240 tracks, allowing scientists to see how glaciers and other frozen features change 26 00:01:41.260 --> 00:01:45.270 with the seasons, including over winter. A 3-D look at Earth. 27 00:01:45.290 --> 00:01:49.320 Now with more height. ICESat-2 will measure elevation to see how much 28 00:01:49.340 --> 00:01:53.360 glaciers, sea ice and ice sheets are rising or falling and give us a more 29 00:01:53.380 --> 00:01:57.390 complete picture of our planet. There are two types of ice that ICESat-2 is after: 30 00:01:57.410 --> 00:02:01.400 land ice and sea ice. Land ice builds up year after year 31 00:02:01.420 --> 00:02:05.430 from snowfall, but sea ice forms when the ocean water freezes. It can last 32 00:02:05.450 --> 00:02:09.470 for years or just one winter. Only one instrument, 33 00:02:09.490 --> 00:02:13.520 but it's a really good one. The Advanced Topographic Laser Altimeter System, 34 00:02:13.540 --> 00:02:17.570 or ATLAS, was built by hundreds of people at NASA's Goddard Space Flight Center 35 00:02:17.590 --> 00:02:21.630 to exacting requirements so that scientists, very soon, can measure 36 00:02:21.650 --> 00:02:25.680 minute changes in our planet's ice. 37 00:02:25.700 --> 00:02:28.375