1 00:00:00,520 --> 00:00:03,560 Speaker 1: Welcome to brain Stuff from house stuff works dot com 2 00:00:03,560 --> 00:00:14,560 Speaker 1: where smart happens. Hi a Marshall brain with today's question, 3 00:00:14,960 --> 00:00:18,959 Speaker 1: how do they measure sea level? An accurate measurement of 4 00:00:19,079 --> 00:00:22,680 Speaker 1: sea level is very hard to pin down. It seems 5 00:00:22,720 --> 00:00:25,840 Speaker 1: like it would be easy, but it's actually quite complicated. 6 00:00:26,200 --> 00:00:30,400 Speaker 1: It's an important measurement though, for two reasons. First, by 7 00:00:30,480 --> 00:00:33,960 Speaker 1: having an accurate sea level measurement, it's possible to measure 8 00:00:33,960 --> 00:00:38,320 Speaker 1: the height of everything on land accurately. Second, by knowing 9 00:00:38,440 --> 00:00:41,559 Speaker 1: sea level, we can determine if the oceans are rising 10 00:00:41,680 --> 00:00:45,720 Speaker 1: or falling over time. The concern is that global warming 11 00:00:45,760 --> 00:00:49,320 Speaker 1: and other weather changes caused by man might be leading 12 00:00:49,320 --> 00:00:52,720 Speaker 1: to an overall rise in sea level. If so, coastal 13 00:00:52,800 --> 00:00:56,600 Speaker 1: cities are in big trouble. The problem with measuring the 14 00:00:56,760 --> 00:00:59,920 Speaker 1: level of the sea is that there are so many 15 00:01:00,120 --> 00:01:03,280 Speaker 1: different things that perturb it. If you could take planet 16 00:01:03,360 --> 00:01:06,000 Speaker 1: Earth and move it out into deep space so that 17 00:01:06,040 --> 00:01:09,080 Speaker 1: the Sun, the Moon, and the other planets didn't affect it, 18 00:01:09,520 --> 00:01:13,960 Speaker 1: and there were no temperature variations worldwide, then everything would 19 00:01:14,000 --> 00:01:18,120 Speaker 1: settle down like a still pond. Rain and wind would stop, 20 00:01:18,160 --> 00:01:21,039 Speaker 1: and so would the rivers. Then you could measure the 21 00:01:21,160 --> 00:01:24,520 Speaker 1: sea level accurately. If you did this, the level of 22 00:01:24,560 --> 00:01:28,240 Speaker 1: the ocean's water projected across the entire planet would be 23 00:01:28,280 --> 00:01:31,319 Speaker 1: called the g oid. On land, you can think of 24 00:01:31,360 --> 00:01:34,280 Speaker 1: the geoid as the level that ocean water would have 25 00:01:34,440 --> 00:01:36,480 Speaker 1: if you were to dig a canal from the ocean 26 00:01:36,680 --> 00:01:40,080 Speaker 1: shore to any point on land. But the Earth is 27 00:01:40,200 --> 00:01:43,000 Speaker 1: not in deep space. It's in the middle of a 28 00:01:43,120 --> 00:01:47,080 Speaker 1: chaotic solar system. There are all sorts of things changing 29 00:01:47,080 --> 00:01:50,760 Speaker 1: the water level at any given point, including the tides 30 00:01:50,880 --> 00:01:54,240 Speaker 1: which are caused by the Moon, large and small waves 31 00:01:54,360 --> 00:01:58,040 Speaker 1: caused by wind and the tides. High and low pressure 32 00:01:58,080 --> 00:02:01,520 Speaker 1: areas in the atmosphere would change the surface level of 33 00:02:01,520 --> 00:02:05,040 Speaker 1: the ocean by pushing or pulling on it, Temperature changes 34 00:02:05,120 --> 00:02:08,200 Speaker 1: in the ocean itself, which changed the density and volume 35 00:02:08,240 --> 00:02:12,160 Speaker 1: of the ocean's water, rainfall and river water flowing into 36 00:02:12,200 --> 00:02:15,040 Speaker 1: the ocean, and so on. If you were to stand 37 00:02:15,160 --> 00:02:17,960 Speaker 1: on the ocean shore and try to measure the sea 38 00:02:18,040 --> 00:02:20,919 Speaker 1: level with a ruler, you would find it to be impossible. 39 00:02:21,240 --> 00:02:24,600 Speaker 1: The level changes by the second from the waves, by 40 00:02:24,639 --> 00:02:27,400 Speaker 1: the hour from the tides, and by the weak from 41 00:02:27,520 --> 00:02:31,440 Speaker 1: planetary and solar orbit changes. To get around all these 42 00:02:31,480 --> 00:02:37,120 Speaker 1: different variations, scientists try using something called tide gauges. A 43 00:02:37,240 --> 00:02:40,760 Speaker 1: tie gauge is a large like one foot in diameter 44 00:02:41,240 --> 00:02:44,400 Speaker 1: and long like ten or twenty or thirty feet long 45 00:02:44,880 --> 00:02:48,520 Speaker 1: pipe with a small hole below the water line. This 46 00:02:48,639 --> 00:02:52,800 Speaker 1: pipe is often called a stilling well. Even though the 47 00:02:52,800 --> 00:02:56,399 Speaker 1: waves are changing the water level outside the gauge constantly, 48 00:02:56,760 --> 00:03:00,280 Speaker 1: they have little effect inside the gauge. The sea level 49 00:03:00,320 --> 00:03:04,480 Speaker 1: can be read relatively accurately inside this pipe. If read 50 00:03:04,520 --> 00:03:07,720 Speaker 1: on a regular basis over a time span of years 51 00:03:07,840 --> 00:03:11,280 Speaker 1: and then average, you can get a good measurement of 52 00:03:11,400 --> 00:03:14,840 Speaker 1: sea level. You can see that getting an accurate reading, 53 00:03:14,960 --> 00:03:18,560 Speaker 1: for example, down to the millimeter level, is extremely difficult. 54 00:03:18,960 --> 00:03:21,680 Speaker 1: Satellites are now used as well, but they suffer from 55 00:03:21,680 --> 00:03:25,080 Speaker 1: many of the same problems. Scientists do the best they can, 56 00:03:25,480 --> 00:03:29,079 Speaker 1: using extremely long time spans to try to figure out 57 00:03:29,120 --> 00:03:32,160 Speaker 1: what this sea level actually is and whether or not 58 00:03:32,280 --> 00:03:36,360 Speaker 1: it is actually rising. The general consensus seems to be 59 00:03:36,440 --> 00:03:40,280 Speaker 1: that the ocean's rise about two millimeters per year. Right now, 60 00:03:41,320 --> 00:03:44,200 Speaker 1: Do you have any ideas or suggestions for this podcast? 61 00:03:44,640 --> 00:03:47,280 Speaker 1: If so, please send me an email at podcast at 62 00:03:47,280 --> 00:03:50,000 Speaker 1: how stuff works dot com. For more on this and 63 00:03:50,080 --> 00:03:52,480 Speaker 1: thousands of other topics, go to how stuff works dot 64 00:03:52,480 --> 00:03:55,320 Speaker 1: com and be sure to check out the brain Stuff 65 00:03:55,320 --> 00:03:57,840 Speaker 1: blog on the house stuffworks dot com home page