1 00:00:00,000 --> 00:00:04,000 [Music] 2 00:00:04,000 --> 00:00:08,000 Narrator: On September 18th 2019, satellites observed that 3 00:00:08,000 --> 00:00:12,000 Arctic sea ice had reached its annual low. 4 00:00:12,000 --> 00:00:16,000 This year's sea ice minimum is effectively tied for the second lowest on record. 5 00:00:16,000 --> 00:00:20,000 And while sea ice grows and shrinks with the seasons, 6 00:00:20,000 --> 00:00:24,000 2019 continues the downward trend of the extent. 7 00:00:24,000 --> 00:00:28,000 Nathan Kurtz: The trends we’ve been seeing 8 00:00:28,000 --> 00:00:32,000 with the sea ice minimum have just been a decrease. 9 00:00:32,000 --> 00:00:36,000 So, in the 70’s since the modern record began tracking to today, 10 00:00:36,000 --> 00:00:40,000 there is variation from year to year, but it’s really just a 11 00:00:40,000 --> 00:00:44,000 a downward trend. Narrator: Satellite observations show that Arctic sea ice 12 00:00:44,000 --> 00:00:48,000 is not only shrinking in extent, it is also becoming younger 13 00:00:48,000 --> 00:00:52,000 and thiner. That means less and less ice survives 14 00:00:52,000 --> 00:00:56,000 the annual melt. Kurtz: The Artic has actually warmed a lot more than 15 00:00:56,000 --> 00:01:00,000 the globe at a whole. There is something called Artic amplification, which means 16 00:01:00,000 --> 00:01:04,000 that the temperatures in the Arctic have warmed about 2 – 3 times 17 00:01:04,000 --> 00:01:08,000 the global average. 18 00:01:08,000 --> 00:01:12,000 Narrator: A major cause of this warming is due to the loss of the reflectivity - or albedo – of the sea ice. 19 00:01:12,000 --> 00:01:16,000 Snow-covered sea ice has a high albedo. This helps keep the 20 00:01:16,000 --> 00:01:20,000 sun’s energy from being absorbed by a dark ocean. 21 00:01:20,000 --> 00:01:24,000 But when sea ice melts, it loses some of that reflectivity. 22 00:01:24,000 --> 00:01:28,000 And without the sea ice cover, the ocean will absorb most 23 00:01:28,000 --> 00:01:32,000 of the sun’s energy. 24 00:01:32,000 --> 00:01:36,000 This creates a feedback loop that leads to more melting and warming in the Arctic. 25 00:01:36,000 --> 00:01:40,000 Kurtz: We care about sea ice for a variety of reasons. 26 00:01:40,000 --> 00:01:44,000 One being is because it does have an impact on things like our weather and our climate. 27 00:01:44,000 --> 00:01:48,000 Because of the albedo effect if you decrease the amount of sea ice 28 00:01:48,000 --> 00:01:52,000 you start warming up the Arctic, and when you start warming up the Arctic 29 00:01:52,000 --> 00:01:56,000 you start changing the circulating of the jet stream which brings 30 00:01:56,000 --> 00:02:00,000 weather to us here in the mid latitudes. 31 00:02:00,000 --> 00:02:04,000 Other reasons why we care about sea ice, Arctic sea ice in particular, 32 00:02:04,000 --> 00:02:08,000 Because we’ve such big changes due to warming 33 00:02:08,000 --> 00:02:12,000 melting ice, it is a good visual to show that, yes, the climate 34 00:02:12,000 --> 00:02:16,000 Is changing and it is because of warming. 35 00:02:16,000 --> 00:02:20,000 Narrator: NASA continues to monitor these changes to the Arctic so that we may get a better 36 00:02:20,000 --> 00:02:24,000 understanding of what we can expect in the future. 37 00:02:24,000 --> 00:00:NaN,000 [Music]