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