2 00:00:02,440 --> 00:00:16,470 A different way of measuring the temperature is over the ocean. 4 00:00:16,470 --> 00:00:20,250 And this is good because it doesn't have any possibility of 5 00:00:20,250 --> 00:00:24,000 an urban heat island effect and so it's a separate check. 6 00:00:24,000 --> 00:00:28,450 But there has been a change in the way that temperatures have been measured at 7 00:00:28,450 --> 00:00:35,300 sea over time. In in old times they would cast 8 00:00:35,300 --> 00:00:39,680 a bucket over the side on a rope and then pull a 9 00:00:39,680 --> 00:00:43,590 bucket full of sea water on deck and stick a thermometer in it. 10 00:00:43,590 --> 00:00:49,140 And this had the possibility of bias, because water 11 00:00:49,140 --> 00:00:53,870 on the outside of the bucket could evaporate and could cool that bucket down 12 00:00:53,870 --> 00:01:00,200 just a bit relative to what it was in the actual water that the boat is floating in. 13 00:01:00,200 --> 00:01:04,190 In the mid '40s, there was a transition in the sea surface 15 00:01:04,190 --> 00:01:08,090 temperature data toward measurements that were made 16 00:01:08,090 --> 00:01:11,930 on the cooling water intake to the engine. 17 00:01:11,930 --> 00:01:15,720 They have to bring water in to cool down the engine as it's running, 18 00:01:15,720 --> 00:01:17,390 you measure the temperature as the water 19 00:01:17,390 --> 00:01:20,000 comes in, before you've dumped heat into it. 20 00:01:20,000 --> 00:01:22,330 And that can tell you a sea surface temperature. 21 00:01:22,330 --> 00:01:26,000 Of course this cooling intake might be coming in from a little 22 00:01:26,000 --> 00:01:29,640 bit below the surface; it may not be exactly the same temperature as here. 23 00:01:31,640 --> 00:01:38,680 To put together the land and the sea surface temperature records. 24 00:01:38,680 --> 00:01:40,380 you can't just compare them directly 25 00:01:40,380 --> 00:01:42,740 because they're different quantities. 26 00:01:42,740 --> 00:01:46,440 The land tends to heat up more than the ocean would 27 00:01:46,440 --> 00:01:49,430 the same reason as this urban heat island effect. 28 00:01:49,430 --> 00:01:51,410 The ocean would be like a super 29 00:01:51,410 --> 00:01:53,910 vegetative place with lots and lots of 30 00:01:53,910 --> 00:01:56,780 capability for water vapor to carry away heat. 31 00:01:56,780 --> 00:02:03,170 And also, the ocean is a big heat sink itself, and so the land surface 32 00:02:03,170 --> 00:02:08,180 is actually expected to warm more quickly than the ocean surface for those reasons. 33 00:02:08,180 --> 00:02:10,490 The way to compare these 34 00:02:10,490 --> 00:02:14,380 different temperatures is within a climate model, 35 00:02:14,380 --> 00:02:16,870 where you impose the temperature 36 00:02:16,870 --> 00:02:21,350 at the sea surface from the measured ship data, 37 00:02:21,350 --> 00:02:23,250 and then you use the model 38 00:02:23,250 --> 00:02:26,370 to calculate, to predict the temperatures 39 00:02:26,370 --> 00:02:31,480 in the atmosphere, both in the air just above the 40 00:02:31,480 --> 00:02:34,280 water, but also, more importantly, over the land. 41 00:02:34,280 --> 00:02:36,740 And then you can compare these model predicted land 42 00:02:37,820 --> 00:02:42,450 temperatures with the actual temperatures measured at those weather stations. 43 00:02:42,450 --> 00:02:45,620 And it turns out that the correction, there was 44 00:02:45,620 --> 00:02:48,980 a significant correction that had to be made between this 45 00:02:48,980 --> 00:02:54,000 technique of measuring sea surface temperature in buckets versus 46 00:02:54,000 --> 00:02:59,470 measuring the sea surface temperatures from from the cooling intakes. 47 00:02:59,470 --> 00:03:03,950 But aside from that, the temperature signals that come 48 00:03:03,950 --> 00:03:07,660 out from this are consistent with those from the after that 49 00:03:07,660 --> 00:03:11,650 correction is made, both the land and the sea surface temperatures 50 00:03:11,650 --> 00:03:15,620 are telling us the same thing about the temperatures of the Earth.