WEBVTT FILE 1 00:00:01.000 --> 00:00:02.480 [Music] 2 00:00:02.480 --> 00:00:06.480 Narrator: It is easy to imagine Greenland as a land of perpetual ice. 3 00:00:06.480 --> 00:00:09.000 However, scientists have recently estimated that the Greenland Ice Sheet may 4 00:00:09.000 --> 00:00:13.000 be gone within the millennium. 5 00:00:13.000 --> 00:00:17.000 Andy: My name is Andy Aschwanden, I am a Glaciologist with the University 6 00:00:17.000 --> 00:00:20.000 of Alaska, Fairbanks. I work at the Geophysical Institute. 7 00:00:20.000 --> 00:00:24.000 Narrator: Andy and his colleagues have used data 8 00:00:24.000 --> 00:00:27.000 collected by NASA to model some of the possible futures of the Greenland Ice Sheet. 9 00:00:27.000 --> 00:00:31.000 Andy: So, we see our projection 10 00:00:31.000 --> 00:00:34.000 of how the Greenland Ice Sheet will retreat 11 00:00:34.000 --> 00:00:37.000 over the course of the next roughly 300 years. 12 00:00:37.000 --> 00:00:41.000 It’s really cool that now we can actually watch 13 00:00:41.000 --> 00:00:45.000 in the animation, in the simulation, how we think it behaves. 14 00:00:45.000 --> 00:00:48.000 I mean, we put the best physics possible in there and we can 15 00:00:48.000 --> 00:00:52.000 actually watch what could happen. That is something we could not have done before. 16 00:00:52.000 --> 00:00:55.000 NASA’s Operation Ice Bridge 17 00:00:55.000 --> 00:00:58.000 over the past decade has been instrumental in gathering the 18 00:00:58.000 --> 00:01:02.000 datasets that help drive our model. 19 00:01:02.000 --> 00:01:06.000 Narrator: This model gives us a more accurate picture of how greenhouse gas 20 00:01:06.000 --> 00:01:10.270 emissions may affect Greenland - and us - in the future. 21 00:01:10.270 --> 00:01:14.000 Andy: Of the three scenarios that we tested there was one sort 22 00:01:14.000 --> 00:01:17.000 of a low emissions, medium emissions, 23 00:01:17.000 --> 00:01:24.000 and high emission scenario. And, 24 00:01:24.000 --> 00:01:28.000 at the moment, it looks like we’re on the highest scenario. 25 00:01:28.000 --> 00:01:31.000 The three different scenarios lead to 26 00:01:31.000 --> 00:01:34.000 basically three different futures, three different Greenlands. 27 00:01:34.000 --> 00:01:38.000 If we choose the path we are on right now, 28 00:01:38.000 --> 00:01:42.000 if we stay on that path, there is actually good chance that within 1000 29 00:01:42.000 --> 00:01:45.000 years or so, the whole Ice Sheet 30 00:01:45.000 --> 00:01:48.000 will be gone. 31 00:01:48.000 --> 00:01:55.000 Narrator: These scenarios show that the melting ice could contribute at least 80% more sea level rise than previous estimates. 32 00:01:55.000 --> 00:01:57.000 This model helps us understand the dynamic nature of the Greenland 33 00:01:57.000 --> 00:02:12.736 Ice Sheet, and arms us with the knowledge we need to inform our future.