How Do Oceans Circulate? Crash Course Geography #9 - By Math and Science
Transcript
00:0-1 | Welcome to the North pacific garbage patch , the largest | |
00:02 | human trash dump in the world spreading across the pacific | |
00:05 | ocean . The North pacific garbage patch is really more | |
00:07 | of a series of trash vortices and is the top | |
00:10 | vacation destination for plastic chemical sludge and wood pulp , | |
00:13 | defining its size is difficult because it's always moving and | |
00:16 | it's mostly a soup of tiny micro plastics , not | |
00:18 | an island of grocery bags and drinking straws , But | |
00:21 | some scientists estimate it's approximately 700,000 km2 , which is | |
00:25 | roughly the size of Texas . Actually , it's one | |
00:27 | of five giant collections of trash circulating in oceans all | |
00:31 | over the earth . If you've spent time on beaches | |
00:32 | , you might have noticed plastic trash like water bottles | |
00:35 | and toys . But there's so much almost invisible junk | |
00:37 | to like small beads or tiny slivers . Each beach | |
00:41 | around the world has this plastic pollution because of how | |
00:43 | trash moves from inland to the ocean and then gets | |
00:45 | caught in ocean currents . Whether you live on a | |
00:47 | coast or not , everyone is connected to global ocean | |
00:50 | currents circulating tremendous amounts of energy and trash . I'm | |
00:53 | al is a career and this is crash course geography | |
01:04 | Somehow trash can show up on a beach in California | |
01:06 | from a pot of trash 2500 nautical miles away east | |
01:09 | of Hawaii . That's so far for one speck of | |
01:12 | plastic or even a whole water bottle with or without | |
01:14 | the secret message to travel to get there , it | |
01:17 | all starts with the wind . In our last episode | |
01:19 | , we explored how the horizontal movement of air , | |
01:21 | called wind moves in predictable directions and creates the general | |
01:24 | patterns for global circulation in the oceans . We call | |
01:27 | the horizontal movement of water and ocean current . Like | |
01:30 | the winds , ocean currents are basically rivers of energy | |
01:33 | moving in a persistent and predictable direction and also like | |
01:36 | the winds . Ocean currents are driven by differences in | |
01:38 | density and pressure in the air density , and pressure | |
01:40 | changes come from differences in the amount of insulation or | |
01:43 | incoming solar radiation that different parts of the atmosphere receive | |
01:46 | . And ocean water is heated by insulation too , | |
01:48 | because of how much direct sunlight it gets . Water | |
01:51 | closer to the equator absorbs more heat energy than water | |
01:54 | at higher latitudes . This creates density differences within the | |
01:56 | ocean because just like air , warm water is less | |
01:59 | dense than cold water basically . When heated molecules like | |
02:02 | to spread out , water density is also affected by | |
02:05 | salinity or the salt content of the water . Saltier | |
02:07 | water is more dense than less salty water because there | |
02:09 | are more molecules of salt and water hanging around . | |
02:12 | Warmer water in the ocean expands just like air , | |
02:14 | but because it can't expand sideways because , you know | |
02:17 | , there's already water there . It expands up , | |
02:19 | elevating the surface just slightly like a hill and colder | |
02:22 | or saltier water contracts , lowering the surface into a | |
02:25 | depression so the ocean's surface isn't perfectly flat . It | |
02:28 | contains sea surface height anomalies . A hill of water | |
02:31 | exerts extra pressure compared to a dip in the sea | |
02:33 | surface height and in general , whatever is in a | |
02:35 | high pressure area , whether it's air or water or | |
02:38 | a student and stressful class wants to move to a | |
02:40 | low pressure area . So these pressure gradients force the | |
02:43 | water to flow around the globe . Technically it's all | |
02:45 | the same water but separate currents are defined because they | |
02:48 | consistently move in the same way , kind of like | |
02:50 | different highways of water . There are actually 30 major | |
02:53 | named surface currents and dozens more smaller currents transporting ocean | |
02:56 | water around the globe . So if our trash found | |
02:59 | its way to the right spot , it could travel | |
03:01 | the world . We can draw lots of comparisons between | |
03:03 | ocean currents and wind patterns , but surface currents are | |
03:06 | also driven by strong and steady streams of wind . | |
03:09 | Energy is transferred from the winds to the water through | |
03:11 | friction as air blows across the surface . For example | |
03:14 | , the winds that result from subtropical high pressure areas | |
03:16 | around 30° latitude also helped create the ocean currents that | |
03:20 | circulate there in patterns called Gyres . But even though | |
03:22 | ocean currents generally follow the winds , the two aren't | |
03:25 | mere images . Ocean currents come up against huge roadblocks | |
03:28 | that air blows right over continents and large land masses | |
03:32 | . These roadblocks give current irregular shapes , especially in | |
03:34 | places like the indian ocean , the arctic ocean and | |
03:37 | the northern atlantic ocean , where there's lots of land | |
03:39 | currents are also curved by the Coriolis effect . Like | |
03:42 | all fluids on the Earth's surface . Remember the Earth | |
03:45 | is rotating fastest at the equator and slower as we | |
03:47 | move towards the poles . So if something that's not | |
03:49 | directly connected to land moves north or south , the | |
03:52 | change in momentum causes its path to bend . The | |
03:54 | Coriolis effect can actually deflect some surface currents depending on | |
03:57 | where they are on the globe . Like as currents | |
04:00 | move away from the equator , the Coriolis effect gets | |
04:02 | stronger because the Earth's rotational speed rapidly slows down and | |
04:06 | can break up currents into chains of lots of circular | |
04:08 | vortices for Eddie's . These get smaller , the closer | |
04:11 | you are to the polls as the coriolis effect bends | |
04:13 | the currents ever more tightly . Then , as the | |
04:15 | earth rotates faster as we move towards the equator , | |
04:18 | the Coriolis effect gets weakest until it's basically non existent | |
04:21 | , exactly at the equator . So equatorial currents aren't | |
04:24 | deflected right or left . Water can simply flow in | |
04:26 | a straight direction , pushed by the winds . So | |
04:28 | if we look at the circulation map , most of | |
04:30 | the surface currents making up gyres don't cross the equator | |
04:33 | but flow along at horizontally . Then it's the combined | |
04:36 | forces of winds and the Coriolis effect that causes gyres | |
04:39 | to flow in a clockwise direction in the northern hemisphere | |
04:41 | and a counter clockwise direction in the southern hemisphere . | |
04:44 | But let's go back to the idea that ocean currents | |
04:46 | not only run into stuff like land , they can | |
04:48 | also carry more stuff than wind . Maybe they're a | |
04:51 | highway for eel migration or they play a role in | |
04:53 | a water bottles journey from a store shelf to the | |
04:55 | north pacific garbage patch . At some point , this | |
04:57 | bottle got snagged in the north pacific gyre , which | |
04:59 | is really four currents that follow how the air moves | |
05:02 | around the northern subtropical high pressure area . To imagine | |
05:05 | its journey , let's go to the thought bubble , | |
05:06 | let's say , our water bottle fell into a municipal | |
05:08 | storm drain in Hawaii . They got flushed into the | |
05:10 | pacific ocean starting at the equator . The trade winds | |
05:13 | drive water west in a flow called the equatorial current | |
05:16 | , This carries our water bottle to the eastern coastline | |
05:18 | of Asia , where warm waters pile up against the | |
05:21 | land , so the warm energy rich waters are deflected | |
05:23 | towards the north pole , pushed by both pressure gradients | |
05:26 | and the coriolis effect that balance each other out . | |
05:28 | They flow into the Kuroshio current moving north along the | |
05:31 | Asian east coast , where our bottle could wave at | |
05:33 | the Philippines in japan . You know if water bottles | |
05:36 | at arms as it reaches the latitude of the westerly | |
05:38 | winds around 35° North , the current begins to wobble | |
05:41 | more , and along with our bottle is pushed eastward | |
05:43 | and separates from the coast . This forms the North | |
05:46 | Pacific current , bringing warm waters to the southern coast | |
05:49 | of Alaska and then land . Hope . Eventually , | |
05:51 | our water bottle encounters the west coast of North America | |
05:54 | and is deflected back towards the equator . Moving from | |
05:56 | british Columbia Canada to the baja peninsula in Mexico . | |
06:00 | This California current is cold having released the warmth that | |
06:03 | the water was holding in the equatorial and Kuroshio currents | |
06:06 | . If the bottle manages to stay in the gyre | |
06:07 | , it could float on through those warm and cold | |
06:09 | currents for years , traveling through clear moonlit nights and | |
06:13 | rough typhoons because our bottle is a processed plastic bacteria | |
06:16 | don't eat away at it , but wind waves and | |
06:18 | sunlight have broken it down into microscopic particles . So | |
06:21 | all that's left is a bead that ends up floating | |
06:23 | in the north pacific garbage patch . Thanks that bubble | |
06:26 | wind current interactions are actually much more complicated than just | |
06:30 | winds pushing water around and it's an area oceanographers are | |
06:33 | still trying to understand for geographers were concerned with how | |
06:36 | stuff gets moved around the globe . There are actually | |
06:38 | five major gyres in the world , including this north | |
06:41 | pacific gyre , each with its own garbage patch . | |
06:43 | And they all follow similar patterns with warm currents bringing | |
06:46 | warmth and humidity to the continental east coasts , and | |
06:48 | cold currents , moderating temperatures and having a drying effect | |
06:51 | on the West Coast . Ocean circulation in the southern | |
06:54 | hemisphere is similar , except that the gyres flow in | |
06:56 | a counterclockwise direction . And because there's very little land | |
06:59 | polar to 40°, South the antarctic Circumpolar current , or | |
07:03 | west wind drift circles around Antarctica as a cold current | |
07:06 | almost without interruption or directly interacting with the warm equatorial | |
07:10 | waters . Surface currents generally move warm waters , poll | |
07:12 | word , and cold waters toward the equator . So | |
07:14 | they're important regional air temperature regulators , in addition to | |
07:18 | moving anything that happens to be in the ocean from | |
07:20 | schools of fish to bits of plastic . But surface | |
07:22 | currents don't make up all of the horizontal motion of | |
07:24 | the ocean . To see the rest , we have | |
07:27 | to go deep into the ocean . Deep currents travel | |
07:29 | at slower speeds beneath the surface currents . They move | |
07:32 | ocean waters both horizontally across the floors of the world's | |
07:34 | oceans , but also vertically from the ocean floor to | |
07:37 | the bottom of surface currents as part of earth's thermal | |
07:39 | . Hey line circulation , just like surface currents , | |
07:41 | deep currents flow from high pressure to low pressure . | |
07:44 | Even at these crushing depths , slight pressure and density | |
07:47 | differences are also caused by temperature and salinity changes . | |
07:50 | For example , the more salt content the surface water | |
07:52 | has , the more dense it is , the more | |
07:54 | likely it will sink as it reaches the polls . | |
07:56 | In some places , that water will sink up to | |
07:58 | 2000 m to where deep currents flow . A complete | |
08:01 | circuit of a deep current may take up to 1000 | |
08:04 | years . Even still , deep currents are critical to | |
08:06 | the movement of nutrients around the world . Many fisheries | |
08:09 | , for example , depend on cyclical upwelling of nutrient | |
08:12 | rich water moving from deep currents into local surface currents | |
08:14 | , while nutrients released through decomposition near the ocean floor | |
08:17 | are pulled up by upwelling oxygen cycles down from the | |
08:20 | surface to the deep , Which keeps those d composers | |
08:22 | and other deep sea organisms supplied with oxygen for respiration | |
08:25 | . So the broad global circulation of deep currents is | |
08:28 | like a vast conveyor belt of ocean water that brings | |
08:30 | warmth from the equator to the poles , nutrients from | |
08:33 | the floor to the surface and oxygen from the surface | |
08:35 | to the floor . Marine habitats near upwelling only cover | |
08:38 | about 1% of Earth's oceans , but account for up | |
08:40 | to 50% of the global fish harvest . At least | |
08:43 | a billion people rely on fish for their primary protein | |
08:46 | . So deep ocean circulation not only moves energy around | |
08:48 | the globe , but also helps create the conditions that | |
08:51 | feed a large part of the world . Higher up | |
08:53 | dominant winds and surface currents have helped move people around | |
08:55 | the globe for thousands of years . With the movement | |
08:58 | of ships has come the movement of people and the | |
08:59 | things they deem most important . We can understand the | |
09:02 | material culture of a people by the marine debris . | |
09:04 | They create . Some of that trash will get swept | |
09:06 | into regional surface currents like gyres , but some will | |
09:09 | get caught by smaller local currents and wash up on | |
09:11 | the shore without having traveled the world . Like , | |
09:13 | there have been outbreaks of whole toys washing up on | |
09:15 | beaches from rubber ducks to lego dragons to Garfield phones | |
09:19 | . What do all of these things have in common | |
09:21 | ? Well , like you've probably intuited marine debris in | |
09:24 | the 21st century is mostly plastic . There are eight | |
09:26 | million metric tons of plastic bits and debris that we | |
09:29 | don't know the origin of , or non point source | |
09:31 | pollution . That's estimated to be in the oceans , | |
09:33 | but there's also bigger garbage out there to take that | |
09:36 | whole lego dragon . It didn't travel far . It | |
09:38 | came from a wrecked shipping container that fell into the | |
09:40 | ocean after a huge once in a 100 years wave | |
09:43 | hit the cargo ship that was carrying it . In | |
09:45 | fact , there are thousands of shipping containers each year | |
09:47 | that fall off cargo ships due to rough weather or | |
09:50 | other mishaps . This map shows the movement of the | |
09:52 | 50,000 ships each day moving goods around the globe . | |
09:55 | Some estimates say 90% of global trade involves container ships | |
09:58 | crossing the oceans , but his ships move , they're | |
10:01 | emitting air pollution that rides on global air circulation currents | |
10:03 | through the atmosphere or dropping stuff that contributes to ocean | |
10:06 | pollution . These types of pollution can't be linked to | |
10:08 | a particular ship because air and water across political boundaries | |
10:11 | . In fact , those plastic beads and dragons on | |
10:13 | the beach represent how we're all connected by the global | |
10:16 | circulation of air and water and how garbage patches won't | |
10:19 | clean themselves are . Global economies depend on the circulation | |
10:22 | of goods moved by ships , and local economies depend | |
10:24 | on the circulation of nutrients that create rich fisheries , | |
10:27 | all of which leveraged the dependability of ocean currents . | |
10:30 | So who's responsible for cleaning international waters ? And how | |
10:33 | do we balance our societal needs with protecting the planet | |
10:36 | ? There aren't easy answers . And there might be | |
10:38 | rough seas ahead . In fact , I see some | |
10:40 | clouds on the horizon . Thanks for watching this episode | |
10:43 | of Crash Course Geography , which was made with the | |
10:45 | help of all these nice people . If you want | |
10:47 | to keep crash course free for everyone forever , you | |
10:49 | can join our community on Patreon . Yeah . |
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