1 00:00:01,840 --> 00:00:07,640 Speaker 1: Welcome to Brainstuff, a production of iHeartRadio, Hey brain Stuff 2 00:00:07,720 --> 00:00:12,640 Speaker 1: Lauren vogelbaumb Here, someone gazing out at the ocean from 3 00:00:12,720 --> 00:00:16,160 Speaker 1: the coast of Maine might see deep, navy to midnight 4 00:00:16,200 --> 00:00:20,200 Speaker 1: blue water, very different hues than someone squinting at the 5 00:00:20,200 --> 00:00:23,560 Speaker 1: bright turquoise sea from a sunny beach on a Greek island. 6 00:00:24,440 --> 00:00:27,760 Speaker 1: So why is the ocean blue? And why does it 7 00:00:27,800 --> 00:00:32,080 Speaker 1: come in so many different shades? Before the article this 8 00:00:32,120 --> 00:00:34,400 Speaker 1: episode is based on how Stuff Work, spoke with NASA 9 00:00:34,479 --> 00:00:39,400 Speaker 1: oceanographer Jean Carl Feldman, who pointed out that, first of all, quote, 10 00:00:39,760 --> 00:00:42,479 Speaker 1: the water of the ocean is not blue, it's clear. 11 00:00:43,159 --> 00:00:45,240 Speaker 1: The color of the ocean's surface, for the most part, 12 00:00:45,440 --> 00:00:48,519 Speaker 1: is based on depth, what's in it and what's below it. 13 00:00:51,000 --> 00:00:54,560 Speaker 1: That's right. All water is clear by its nature. But 14 00:00:54,680 --> 00:00:57,160 Speaker 1: here's why it looks different in a glass versus from 15 00:00:57,160 --> 00:01:00,720 Speaker 1: a beach. A glass of water appears clear because light 16 00:01:00,800 --> 00:01:04,320 Speaker 1: passes through it with little to no obstruction. But if 17 00:01:04,319 --> 00:01:06,720 Speaker 1: a body of water is deep enough that light isn't 18 00:01:06,720 --> 00:01:12,360 Speaker 1: reflected off the bottom, it appears blue. Basic physics explains 19 00:01:12,400 --> 00:01:15,319 Speaker 1: why a visible light is made up of a spectrum 20 00:01:15,319 --> 00:01:18,680 Speaker 1: of different wavelengths The longer wavelengths appear to our eyes 21 00:01:18,720 --> 00:01:21,399 Speaker 1: as shades of red and orange, while the shorter ones 22 00:01:21,440 --> 00:01:25,160 Speaker 1: appear as blues and violets. When light strikes the ocean, 23 00:01:25,480 --> 00:01:28,800 Speaker 1: it interacts with water molecules and can be either absorbed 24 00:01:28,920 --> 00:01:33,240 Speaker 1: or scattered. If nothing is in the water except water molecules, 25 00:01:33,680 --> 00:01:36,840 Speaker 1: the longer red portions of the spectrum are absorbed by 26 00:01:36,840 --> 00:01:41,200 Speaker 1: the water. The shorter, zippier blue wavelengths are more likely 27 00:01:41,240 --> 00:01:44,800 Speaker 1: to hit something, including water and scatter, meaning they make 28 00:01:44,840 --> 00:01:49,000 Speaker 1: it back to our eyes, meaning the ocean appears blue. 29 00:01:49,200 --> 00:01:52,600 Speaker 1: Violet wavelengths are even shorter in zippier, but there are 30 00:01:52,640 --> 00:01:55,240 Speaker 1: fewer of them in sunlight, and our eyes perceive the 31 00:01:55,240 --> 00:02:00,840 Speaker 1: blue ones better at long distances, like near the horizon. 32 00:02:01,080 --> 00:02:03,560 Speaker 1: Another factor that we've actually talked about in a different 33 00:02:03,560 --> 00:02:07,360 Speaker 1: episode comes into play. A mountains appear blue in the 34 00:02:07,360 --> 00:02:10,040 Speaker 1: distance no matter what color they are up close, because 35 00:02:10,080 --> 00:02:12,680 Speaker 1: the air itself is made up of molecules that scatter 36 00:02:12,919 --> 00:02:16,840 Speaker 1: those zippy blue wavelengths of light, so the ocean far 37 00:02:16,840 --> 00:02:19,120 Speaker 1: out in the distance may look bluer than the water 38 00:02:19,320 --> 00:02:23,280 Speaker 1: near a beach. The depth of the water and what 39 00:02:23,360 --> 00:02:26,639 Speaker 1: the ocean floor is made of also influence this, A 40 00:02:26,720 --> 00:02:30,680 Speaker 1: Feldman explained in Grease, the water is this beautiful turquoise 41 00:02:30,680 --> 00:02:33,960 Speaker 1: color because the bottom is either white sand or white rocks. 42 00:02:36,120 --> 00:02:38,680 Speaker 1: What's happening here is that the light hits the shallow 43 00:02:38,720 --> 00:02:42,239 Speaker 1: sea floor and then bounces back up, projecting the beautiful 44 00:02:42,280 --> 00:02:45,679 Speaker 1: blue green color you see in the water. It's particularly 45 00:02:45,720 --> 00:02:48,600 Speaker 1: bright because some of those beaches have very little stuff 46 00:02:48,639 --> 00:02:52,840 Speaker 1: in the water, but the ocean is often teeming with 47 00:02:53,000 --> 00:02:57,280 Speaker 1: tiny planted animal life or fulfilled with suspended sediment or containinents. 48 00:02:58,360 --> 00:03:02,040 Speaker 1: Oceanographers monitor the ocean color as doctors read the vital 49 00:03:02,080 --> 00:03:05,240 Speaker 1: signs of their patients. The color seen on the ocean's 50 00:03:05,280 --> 00:03:09,280 Speaker 1: surface reflects what's going on in its vast depths pun intended. 51 00:03:10,960 --> 00:03:13,440 Speaker 1: A Feldman, who is based at the NASA Goddard Space 52 00:03:13,480 --> 00:03:16,880 Speaker 1: Flight Center in Maryland, studies images taken by the Sea 53 00:03:17,000 --> 00:03:20,440 Speaker 1: Viewing Wide Field of View Sensor satellite, which launched back 54 00:03:20,440 --> 00:03:23,880 Speaker 1: in nineteen ninety seven. From its orbit more than four 55 00:03:23,960 --> 00:03:26,760 Speaker 1: hundred miles or six hundred and fifty kilometers above Earth, 56 00:03:27,200 --> 00:03:30,919 Speaker 1: the satellite captures van go like swirls of the ocean's colors. 57 00:03:31,800 --> 00:03:35,040 Speaker 1: The patterns are not only mesmerizing, but they also show 58 00:03:35,080 --> 00:03:38,000 Speaker 1: where sediment and runoff may make the water appure a 59 00:03:38,120 --> 00:03:42,880 Speaker 1: muddy brown color, or where microscopic plants called phytoplankton collected 60 00:03:42,960 --> 00:03:48,480 Speaker 1: nutrient rich waters and tinting it green. Phytoplankton use chlorophyll, 61 00:03:48,520 --> 00:03:50,960 Speaker 1: which is a green pigment, to capture energy from the 62 00:03:51,000 --> 00:03:54,160 Speaker 1: sun to convert water in carbon dioxide into food to 63 00:03:54,280 --> 00:03:59,560 Speaker 1: fuel themselves. Through this process called photosynthesis, phytoplankton generate about 64 00:03:59,600 --> 00:04:03,400 Speaker 1: half of the oxygen we breathe. While most phytoplankton give 65 00:04:03,480 --> 00:04:06,760 Speaker 1: ocean water a green tint, some lend it a yellow, reddish, 66 00:04:06,840 --> 00:04:11,920 Speaker 1: or brown tint. Oceans with high concentrations of phytoplankton can 67 00:04:11,920 --> 00:04:16,400 Speaker 1: appear blue green to green, depending on the density. Greenish 68 00:04:16,400 --> 00:04:19,680 Speaker 1: water may not sound appealing, but as Feldman says, if 69 00:04:19,680 --> 00:04:24,080 Speaker 1: it weren't for phytoplankton, we wouldn't be here. Phytoplanktons serve 70 00:04:24,160 --> 00:04:26,560 Speaker 1: as the base of the ocean's food web because they're 71 00:04:26,560 --> 00:04:29,400 Speaker 1: the primary source of food for zooplankton, which are tiny 72 00:04:29,440 --> 00:04:32,200 Speaker 1: animals that are eaten by fish. The fish are then 73 00:04:32,200 --> 00:04:37,039 Speaker 1: eaten by bigger animals like whales and sharks. But when 74 00:04:37,080 --> 00:04:40,720 Speaker 1: oceans become polluted with runoff, the amount of phytoplankton can 75 00:04:40,880 --> 00:04:46,040 Speaker 1: escalate to unhealthy levels. Phytoplankton feed on the pollutants, flourish 76 00:04:46,279 --> 00:04:49,359 Speaker 1: and then die in huge numbers, sinking to the bottom 77 00:04:49,400 --> 00:04:52,679 Speaker 1: and decomposing in a process that depletes oxygen from the water, 78 00:04:53,120 --> 00:04:57,839 Speaker 1: which means larger animals can't survive there. On a map 79 00:04:57,880 --> 00:05:01,000 Speaker 1: on Feldman's office wall is a mark showing a spot 80 00:05:01,040 --> 00:05:03,920 Speaker 1: where there is little human interference and the ocean water 81 00:05:04,160 --> 00:05:08,479 Speaker 1: is perhaps the clearest and cleanest on the planet. In 82 00:05:08,560 --> 00:05:10,839 Speaker 1: this region, off the coast of Easter Island in the 83 00:05:10,839 --> 00:05:14,960 Speaker 1: Southeast Pacific Ocean, the water is deep and remarkably clear 84 00:05:15,200 --> 00:05:17,960 Speaker 1: due to its location in the middle of a giant 85 00:05:17,960 --> 00:05:23,440 Speaker 1: oceanic guyer a large circular current. Its central location means 86 00:05:23,520 --> 00:05:27,159 Speaker 1: there's minimal mixing of ocean layers, and sediment isn't pushed 87 00:05:27,240 --> 00:05:30,599 Speaker 1: up from the deep bottom. The purity of the water here, 88 00:05:30,839 --> 00:05:33,880 Speaker 1: coupled with its depth, make the ocean here appear a 89 00:05:33,920 --> 00:05:39,400 Speaker 1: deeper indigo than perhaps anywhere else. Feldman said, the light 90 00:05:39,640 --> 00:05:43,719 Speaker 1: just keeps going down, down, down, There's nothing that bounces aback. 91 00:05:44,440 --> 00:05:50,520 Speaker 1: Here is the deepest blue you'll ever see. That being said, 92 00:05:50,640 --> 00:05:53,520 Speaker 1: of course, light doesn't just keep going down into the 93 00:05:53,520 --> 00:05:57,440 Speaker 1: water forever. Eventually the water absorbs all of it and 94 00:05:57,520 --> 00:05:59,520 Speaker 1: nothing is left to bounce back up to the surface. 95 00:05:59,600 --> 00:06:03,280 Speaker 1: Band our eyes. Over half of all visible light is 96 00:06:03,320 --> 00:06:05,960 Speaker 1: absorbed within the first ten meters or thirty feet of 97 00:06:06,000 --> 00:06:09,000 Speaker 1: water at the ocean's surface. At one hundred meters or 98 00:06:09,080 --> 00:06:11,880 Speaker 1: three hundred feet, ninety nine percent of light will have 99 00:06:11,880 --> 00:06:16,400 Speaker 1: been absorbed. Even in very clear water. That's where you 100 00:06:16,440 --> 00:06:20,080 Speaker 1: get that deep indigo off Easter Island. All of the longer, 101 00:06:20,160 --> 00:06:26,560 Speaker 1: slower wavelengths have been absorbed, leaving only the darkest violet blue. However, 102 00:06:26,720 --> 00:06:30,479 Speaker 1: at about twice that depth, light never penetrates, and everything 103 00:06:30,480 --> 00:06:34,200 Speaker 1: that lives there lives in total darkness unless they create 104 00:06:34,240 --> 00:06:42,880 Speaker 1: their own light through by aluminescence. But that's a different episode. 105 00:06:43,600 --> 00:06:45,919 Speaker 1: Today's episode is based on the article why is the 106 00:06:45,920 --> 00:06:48,920 Speaker 1: ocean different colors in different places? On HowStuffWorks dot Com? 107 00:06:49,000 --> 00:06:52,040 Speaker 1: Written by Amanda Onion. Rain Stuff is production by Heart 108 00:06:52,120 --> 00:06:54,479 Speaker 1: Radio in partnership with how Stuffworks dot Com and is 109 00:06:54,480 --> 00:06:57,840 Speaker 1: produced by Tyler Klang. Four more podcasts fy Heart Radio, 110 00:06:58,120 --> 00:07:00,920 Speaker 1: visit the iHeartRadio app, Apple podcast Guests, or wherever you 111 00:07:00,960 --> 00:07:02,239 Speaker 1: listen to your favorite shows