1 00:00:01,010 --> 00:00:05,010 [music] 2 00:00:05,010 --> 00:00:09,010 Gardner: The track we’re looking at today passed very 3 00:00:09,010 --> 00:00:13,000 close to the summit of Everest. It was only about 640 meters from the summit. 4 00:00:13,000 --> 00:00:17,000 Now one of the unique things about ICESat-2 is it’s actually able to see down into 5 00:00:17,000 --> 00:00:21,000 the valleys of these very steep topography areas where the glaciers 6 00:00:21,000 --> 00:00:25,000 are. And so there’s other instruments, like radar, that aren’t able to see the glaciers 7 00:00:25,000 --> 00:00:29,000 all the way down in the valleys. And so ICESat-2 is going to let us measure 8 00:00:29,000 --> 00:00:33,000 the changes in mountain glaciers so we can assess how they’re responding to changes in 9 00:00:33,000 --> 00:00:37,000 climate and what potential they have to contribute to sea level rise in the future 10 00:00:37,000 --> 00:00:41,010 but also changes in water resources. Glaciers in this region 11 00:00:41,010 --> 00:00:45,010 have been experiencing rapid rates of thinning. And that thinning is 12 00:00:45,010 --> 00:00:49,000 in response to changes in climate. Not only are these glaciers thinning, but as they 13 00:00:49,000 --> 00:00:53,000 thin, there’s less force pulling them downward. And that less force pulling them 14 00:00:53,000 --> 00:00:57,010 downward is causing them to actually slow down. So in High Mountain Asia 15 00:00:57,010 --> 00:01:01,010 we actually have glaciers that are thinning and slowing down as they respond to climate. 16 00:01:01,010 --> 00:01:05,010 [music] 17 00:01:05,010 --> 00:01:08,010 [music] 18 00:01:08,010 --> 00:01:08,117