1 00:00:00,000 --> 00:00:04,000 Ice. 2 00:00:04,000 --> 00:00:08,000 You might know that ice plays significant part in climate change.\h 3 00:00:08,000 --> 00:00:12,000 But what about how scientists study it? 4 00:00:12,000 --> 00:00:16,000 The first satellite solely dedicated to collecting information on the world’s ice\h 5 00:00:16,000 --> 00:00:20,000 was the Ice, Cloud, and land Elevation Satellite, better known 6 00:00:20,000 --> 00:00:24,000 as ICESat.\hBut back in 2009,\h 7 00:00:24,000 --> 00:00:28,000 ICESat was decommissioned, and ICESat-2 didn’t launch until nearly 8 00:00:28,000 --> 00:00:32,000 a decade later in 2018. So how did we study ice in the meantime?\h 9 00:00:32,000 --> 00:00:36,000 Enter Operation IceBridge. 10 00:00:36,000 --> 00:00:40,000 NASA’s Operation IceBridge was created to quite literally bridge 11 00:00:40,000 --> 00:00:44,000 the gap in data collection between satellites, and it’s the largest 12 00:00:44,000 --> 00:00:48,000 airborne survey of Earth's polar ice ever.\h 13 00:00:48,000 --> 00:00:52,000 After 11 years of providing invaluable yearly measurements from both poles,\h 14 00:00:52,000 --> 00:00:56,000 surveying glaciers, ice sheets, and sea ice, most of IceBridge came to\h 15 00:00:56,000 --> 00:01:00,000 a close. However, one small part of the mission 16 00:01:00,000 --> 00:01:04,000 still continues in 2020 -- Operation IceBridge 17 00:01:04,000 --> 00:01:08,000 Alaska.\hA team of scientists from the University 18 00:01:08,000 --> 00:01:12,000 of Alaska Fairbanks studies and records the annual changes in Alaska’s 19 00:01:12,000 --> 00:01:16,000 ice thickness. They do so through a remarkable aircraft.\h 20 00:01:16,000 --> 00:01:20,000 specially retrofitted for science. By shooting a laser 21 00:01:20,000 --> 00:01:24,000 out of the bottom of the plane that hits the glacier’s surface and bounces back up, 22 00:01:24,000 --> 00:01:28,000 scientists can measure the surface elevation.\hAnd using ice-penetrating 23 00:01:28,000 --> 00:01:32,000 radar, they can measure the bedrock below the glacier, and come up with 24 00:01:32,000 --> 00:01:36,000 an estimate of ice thickness. But the field missions in Alaska 25 00:01:36,000 --> 00:01:40,000 face especially challenging circumstances. In order 26 00:01:40,000 --> 00:01:44,000 to measure glaciers within data collection lines, the plane must be flown 27 00:01:44,000 --> 00:01:48,000 very low while navigating around extremely tricky mountain ranges, 28 00:01:48,000 --> 00:01:52,000 making for some of the most adventurous mission flying around. 29 00:01:52,000 --> 00:01:56,000 Even the glaciers themselves have proven to be a challenge to scientists.\h 30 00:01:56,000 --> 00:02:00,000 Most glaciers in Alaska are temperate, meaning 31 00:02:00,000 --> 00:02:04,000 they’re at their melting point from surface to base, and contain large pockets 32 00:02:04,000 --> 00:02:08,000 of water within the ice. Those pools of water muddle the 33 00:02:08,000 --> 00:02:12,000 radar signals, making it difficult to collect consistent measurements of 34 00:02:12,000 --> 00:02:16,000 thickness. And these measurements recorded are vital. 35 00:02:16,000 --> 00:02:20,000 Alaskan glaciers make up only a small percentage of the world’s ice,\h 36 00:02:20,000 --> 00:02:24,000 but they contribute a disproportionately large amount to sea level rise. 37 00:02:24,000 --> 00:02:28,000 The research and data collection done\h 38 00:02:28,000 --> 00:02:32,000 under Operation IceBridge helps give scientists a closer look at the 39 00:02:32,000 --> 00:02:36,000 connections between mountain glaciers and global climate change.