1 00:00:09,379 --> 00:00:06,050 as most people know majority the earth 2 00:00:12,199 --> 00:00:09,389 is covered by the oceans they store a 3 00:00:15,260 --> 00:00:12,209 majority of the heat that we get and in 4 00:00:18,800 --> 00:00:15,270 that respect interact with the climate 5 00:00:21,730 --> 00:00:18,810 the ocean is a big sink for heat it can 6 00:00:24,160 --> 00:00:21,740 absorb heat from the atmosphere so if we 7 00:00:27,109 --> 00:00:24,170 continue to warm the atmosphere through 8 00:00:29,990 --> 00:00:27,119 increasing carbon dioxide or other 9 00:00:33,110 --> 00:00:30,000 factors the ocean will absorb that heat 10 00:00:34,580 --> 00:00:33,120 and store it and it can store up to 80 11 00:00:37,660 --> 00:00:34,590 percent of that heat but the question is 12 00:00:39,860 --> 00:00:37,670 will it keep doing that in the future 13 00:00:41,840 --> 00:00:39,870 well the ocean surface topography 14 00:00:44,660 --> 00:00:41,850 mission is important because it provides 15 00:00:46,939 --> 00:00:44,670 a view of the changing climate it 16 00:00:48,529 --> 00:00:46,949 monitors the consequences of global 17 00:00:53,779 --> 00:00:48,539 climate change and global warming by 18 00:00:56,419 --> 00:00:53,789 monitoring sea-level rise half the ward 19 00:01:00,530 --> 00:00:56,429 population lives within 100 kilometre 20 00:01:08,310 --> 00:01:04,710 sea level is rising at 3 millimeters per 21 00:01:10,860 --> 00:01:08,320 year the ice Street of Antarctica and 22 00:01:16,310 --> 00:01:10,870 Greenland each has a capacity of Reason 23 00:01:20,210 --> 00:01:18,110 it's measuring the height of the ocean 24 00:01:22,250 --> 00:01:20,220 surface to a few inches from 800 miles 25 00:01:23,780 --> 00:01:22,260 above the surface of the earth measure 26 00:01:25,610 --> 00:01:23,790 my hand here is the spacecraft in this 27 00:01:27,590 --> 00:01:25,620 ball is the pulse of energy radar energy 28 00:01:28,880 --> 00:01:27,600 that it sends to the surface what it 29 00:01:30,560 --> 00:01:28,890 does is it measures the amount of time 30 00:01:32,600 --> 00:01:30,570 for it to come back if the ocean surface 31 00:01:34,280 --> 00:01:32,610 is lower which is represented by this 32 00:01:36,080 --> 00:01:34,290 lower step here it takes a longer amount 33 00:01:40,910 --> 00:01:36,090 of time to come back than if it were 34 00:01:42,469 --> 00:01:40,920 higher the radar altimeter sends a pulse 35 00:01:43,969 --> 00:01:42,479 of microwave energy down to the surface 36 00:01:46,370 --> 00:01:43,979 and measures the amount of time it takes 37 00:01:48,980 --> 00:01:46,380 to get back it continues the 38 00:01:51,350 --> 00:01:48,990 measurements that were started in 1992 39 00:01:53,600 --> 00:01:51,360 by topex/poseidon and continued with 40 00:01:54,890 --> 00:01:53,610 adjacent one satellite and now we have 41 00:01:56,810 --> 00:01:54,900 the OST M which is going to continue 42 00:01:58,640 --> 00:01:56,820 this record into the future and will 43 00:02:01,460 --> 00:01:58,650 help us answer questions like is sea 44 00:02:04,160 --> 00:02:01,470 level rise going to accelerate OST M is 45 00:02:06,800 --> 00:02:04,170 going to be able to provide us some of 46 00:02:10,040 --> 00:02:06,810 the key information to understanding and 47 00:02:12,650 --> 00:02:10,050 predicting and tracking hurricanes 48 00:02:16,700 --> 00:02:12,660 it's going to be able to provide us same 49 00:02:20,540 --> 00:02:16,710 kind of information for oil rigs for 50 00:02:22,580 --> 00:02:20,550 shipping or fisheries management and 51 00:02:25,450 --> 00:02:22,590 those are some of the very practical 52 00:02:28,160 --> 00:02:25,460 applications besides just the long-term 53 00:02:31,400 --> 00:02:28,170 monitoring of climate it will really