1 00:00:07,030 --> 00:00:04,789 on september 18th 2 00:00:09,910 --> 00:00:07,040 satellites observed that arctic sea ice 3 00:00:11,910 --> 00:00:09,920 had reached its annual low 4 00:00:14,070 --> 00:00:11,920 this year's sea ice minimum is 5 00:00:15,749 --> 00:00:14,080 effectively tied for the second lowest 6 00:00:17,910 --> 00:00:15,759 on record 7 00:00:19,189 --> 00:00:17,920 and while sea ice grows and shrinks with 8 00:00:22,390 --> 00:00:19,199 the seasons 9 00:00:26,790 --> 00:00:22,400 2019 continues the downward trend of the 10 00:00:30,230 --> 00:00:27,990 the trends that we've been seeing with 11 00:00:33,030 --> 00:00:30,240 the sea ice minimum have just been a 12 00:00:35,350 --> 00:00:33,040 decrease so in the 70s since the modern 13 00:00:36,470 --> 00:00:35,360 record began tracking 14 00:00:38,150 --> 00:00:36,480 to today 15 00:00:40,229 --> 00:00:38,160 there's there's variation from year to 16 00:00:41,430 --> 00:00:40,239 year but it's really just a downward 17 00:00:43,510 --> 00:00:41,440 trend 18 00:00:46,389 --> 00:00:43,520 satellite observations show that arctic 19 00:00:49,670 --> 00:00:46,399 sea ice is not only shrinking in extent 20 00:00:52,069 --> 00:00:49,680 it is also becoming younger and thinner 21 00:00:54,470 --> 00:00:52,079 that means less and less ice survives 22 00:00:56,150 --> 00:00:54,480 the annual melt the the arctic is 23 00:00:57,670 --> 00:00:56,160 actually warmed a lot more than the 24 00:00:59,830 --> 00:00:57,680 globe as a whole there's a something 25 00:01:00,709 --> 00:00:59,840 called arctic amplification which means 26 00:01:02,310 --> 00:01:00,719 that 27 00:01:03,910 --> 00:01:02,320 the the temperatures in the arctic have 28 00:01:05,590 --> 00:01:03,920 warmed about two to three times the 29 00:01:07,750 --> 00:01:05,600 global average 30 00:01:10,550 --> 00:01:07,760 a major cause of this warming is due to 31 00:01:13,830 --> 00:01:10,560 the loss of reflectivity or albedo of 32 00:01:16,469 --> 00:01:13,840 the sea ice snow-covered sea ice has a 33 00:01:19,270 --> 00:01:16,479 high albedo this keeps the sun's energy 34 00:01:21,910 --> 00:01:19,280 from being absorbed by a dark ocean 35 00:01:24,390 --> 00:01:21,920 but when sea ice begins to melt it loses 36 00:01:26,870 --> 00:01:24,400 some of that reflectivity 37 00:01:30,149 --> 00:01:26,880 and without the sea ice cover the ocean 38 00:01:32,710 --> 00:01:30,159 will absorb most of the sun's energy 39 00:01:34,630 --> 00:01:32,720 this creates a feedback loop that leads 40 00:01:36,390 --> 00:01:34,640 to more melting and warming in the 41 00:01:38,710 --> 00:01:36,400 arctic 42 00:01:40,390 --> 00:01:38,720 we care about sea ice for a variety of 43 00:01:42,310 --> 00:01:40,400 reasons one being 44 00:01:44,389 --> 00:01:42,320 because it does have an impact on things 45 00:01:46,389 --> 00:01:44,399 like our weather and our climate because 46 00:01:48,469 --> 00:01:46,399 of the albedo effect if you decrease the 47 00:01:50,710 --> 00:01:48,479 amount of arctic sea ice 48 00:01:52,310 --> 00:01:50,720 you start warming up the arctic and when 49 00:01:54,469 --> 00:01:52,320 you start warming up the arctic you can 50 00:01:57,030 --> 00:01:54,479 start changing the circulation of the 51 00:02:00,069 --> 00:01:57,040 the jet stream which brings weather to 52 00:02:02,310 --> 00:02:00,079 us here in the mid-latitudes the other 53 00:02:05,350 --> 00:02:02,320 other reasons why we care about 54 00:02:07,109 --> 00:02:05,360 sea ice arctic sea ice in particular is 55 00:02:09,749 --> 00:02:07,119 because we've seen such big changes due 56 00:02:12,070 --> 00:02:09,759 to warming melting ice it's a 57 00:02:15,430 --> 00:02:12,080 good visual to show that yes the climate 58 00:02:17,589 --> 00:02:15,440 is changing and it's because of warming 59 00:02:19,670 --> 00:02:17,599 nasa continues to monitor these changes 60 00:02:21,350 --> 00:02:19,680 to the arctic so that we may get a