Spreading across the Pacific Ocean, the North Pacific Garbage Patch is really more of a

series of trash vortices and is the top vacation destination for plastic, chemical sludge,

and wood pulp. 

Defining its size is difficult because it's always moving and it's mostly a soup of

tiny microplastics, not an island of grocery bags and drinking straws. But some scientists

estimate it's approximately 700,000 km2, which is roughly the size of Texas.,

Actually, it's one of five giant collections of trash circulating in oceans all over the Earth. 

If you've spent time on beaches, you might've noticed plastic trash like water bottles and

toys, but there's so much almost invisible junk too, like small beads or tiny slivers.

Each beach around the world has this plastic pollution because of how trash moves from

inland to the ocean, and then gets caught in ocean currents. 

Whether you live on a coast or not, everyone is connected to the global ocean currents

circulating tremendous amounts of energy…and trash. 

I'm Alizé Carrère and this is Crash Course Geography.

Intro

Somehow trash can show up on a beach in California from a pod of trash 2500 nautical miles away

east of Hawaii. That's so far for one speck of plastic or even a whole water bottle [-- with

or without the secret message --] to travel. To get there, it all starts with the wind. 

In our last episode, we explored how the horizontal movement of air, called wind, moves in predictable

directions and creates the general patterns for global circulation. In the oceans, we

call the horizontal movement of water an ocean current. 

Like the winds, ocean currents are basically rivers of energy moving in a persistent and

predictable direction. And also like the winds, ocean currents are driven by differences in

density and pressure. 

In the air, density and pressure changes come from differences in the amount of insolation,

or incoming solar radiation, that different parts of the atmosphere receive. 

And ocean water is heated by insolation too. Because of how much direct sunlight it gets,

water closer to the equator absorbs more heat energy than water at higher latitudes. 

This creates density differences within the ocean, because -- just like air -- warm water

is less dense than cold water. Basically when heated, molecules like to spread out. Water

density is also affected by salinity, or the salt content of the water. Saltier water is

more dense than less salty water, because there are more molecules of salt and water

hanging around.

Warmer water in the ocean expands just like air, but because it can't expand sideways

-- because ya know, there's already water there -- it expands up, elevating the surface

just slightly, like a hill. And colder or saltier water contracts, lowering the surface

into a depression. So the ocean's surface isn't perfectly flat. It contains sea surface

height anomalies. 

A “hill” of water exerts extra pressure compared to a dip in the sea surface height.

And in general, whatever's in a high pressure area -- whether it's air or water or a student

in a stressful class -- wants to move to the low pressure area. So these pressure gradients

force the water to flow around the globe.

Technically it's all the same water, but separate currents are defined because they consistently

move in the same way, kind of like different highways of water.

There are actually at least 30 major named surface currents and dozens more smaller currents

transporting ocean water around the globe. So if our trash found its way to the right

spot, it could travel the world!

We can draw lots of comparisons between ocean currents and wind patterns, but surface currents

are also driven by strong and steady streams of wind. Energy is transferred from the winds

to the water through friction as air blows across the surface.

For example, the winds that result from subtropical high pressure areas around 30 degrees latitude

also help create the ocean currents that circulate there in patterns called gyres. 

But even though ocean currents generally follow the winds, the two aren't mirror images.

Ocean currents come up against huge roadblocks that air blows right over: continents and

large land masses. 

These roadblocks give currents irregular shapes, especially in places like the Indian Ocean,

the Arctic Ocean, and the Northern Atlantic Ocean where there's lots of land. 

Currents are also curved by the Coriolis Effect, like all fluids on the Earth's surface.

Remember the Earth is rotating fastest at the equator and slower as we move towards

the poles. So if something that's not directly connected to land moves north or south, the

change in momentum causes its path to bend. 

The Coriolis effect can actually deflect some surface currents, depending on where they

are on the globe. Like, as currents move away from the equator, the Coriolis effect gets

stronger because the Earth's rotational speed rapidly slows down, and can break up

currents into chains of lots of circular vortices, or eddies. These get smaller the closer you

are to the poles as the Coriolis effect bends the currents ever more tightly. 

Then as the Earth rotates faster as we move towards the equator, the Coriolis effect gets

weakest until it's basically nonexistent exactly at the equator. So equatorial currents

aren't deflected right or left -- water can simply flow in a straight direction pushed

by the winds. 

So if we look at the circulation map, most of the surface currents making up gyers don't

cross the equator but flow along it horizontally. Then it's the combined forces of winds and

the Coriolis effect that causes gyres to flow in a clockwise direction in the Northern Hemisphere

and a counterclockwise direction in the Southern Hemisphere. 

But let's go back to the idea that ocean currents not only run into stuff like land,

they can also carry more stuff than wind. Maybe they're a highway for eel migration,

or they play a role in a water bottle's journey from a store shelf to the North Pacific Garbage Patch.

At some point, this bottle got snagged in the North Pacific Gyre, which is really four

currents that follow how the air moves around the northern subtropical high pressure area.

To imagine its journey, let's go to the Thought Bubble.

Let's say our water bottle fell into a municipal storm drain in Hawaii that got flushed into

the Pacific Ocean. 

Starting at the equator, the trade winds drive water west in a flow called the Equatorial Current.

This carries our water bottle to the eastern coastline of Asia, where warm waters pile

up against the land.

So the warm, energy-rich waters are deflected toward the North Pole, pushed by both pressure

gradients and the Coriolis effect that balance each other out.

They flow into the Kuroshio Current moving north along the Asian East Coast, where our

bottle could wave at the Philippines and Japan...you know, if water bottles had arms.

As it reaches the latitude of the westerly winds around 35 degrees north, the current

begins to wobble more, and along with our bottle, is pushed eastward and separates from the coast.

This forms the North Pacific Current, bringing warm waters to the southern coast of Alaska. 

And then, land ho! Eventually our bottle encounters the West Coast of North America and is deflected

back towards the equator, moving from British Columbia, Canada, to the Baja Peninsula in Mexico.

This California Current is cold, having released the warmth that the water was holding in the

Equatorial and Kuroshio currents. 

If the bottle manages to stay in the gyre, it could float on through those warm and cold

currents for years, traveling through clear moonlit nights and rough typhoons. 

Because our bottle is a processed plastic, bacteria don't eat away at it.

But wind, waves, and sunlight have broken it down into microscopic particles, so all

that's left is a bead that ends up floating in the North Pacific Garbage Patch. 

Thanks, Thought Bubble. Wind-current interactions are actually much more complicated than just

winds “pushing” water around, and it's an area oceanographers are still trying to understand.

For geographers, we're concerned with how stuff gets moved around the globe. There are

actually five major gyres in the world, including this North Pacific Gyre, each with its own garbage patch.

And they all follow similar patterns with warm currents bringing warmth and humidity

to the continental east coasts, and cold currents moderating temperatures and having a drying

effect on the west coasts. 

Ocean circulation in the Southern Hemisphere is similar except that the gyres flow in a

counterclockwise direction. And because there's very little land poleward of 40 degrees south,

the Antarctic Circumpolar Current or West Wind Drift circles around Antarctica as a

cold current almost without interruption or directly interacting with the warm equatorial waters.

Surface currents generally move warm waters poleward and cold waters towards the equator,

so they're important regional air temperature regulators in addition to moving anything

that happens to be in the ocean, from schools of fish to bits of plastic! 

But surface currents don't make up all of the horizontal motion of the ocean. To see

the rest, we have to go deep into the ocean.  Deep currents travel at slower speeds beneath

the surface currents. They move ocean waters both horizontally across the floors of the

world's oceans, but also vertically from the ocean floor to the bottom of surface currents

as part of Earth's thermohaline circulation. 

Just like surface currents, deep currents flow from high pressure to low pressure. Even

at these crushing depths, slight pressure and density differences are also caused by

temperature and salinity changes.

For example, the more salt content the surface water has, the more dense it is, the more

likely it will sink as it reaches the poles. In some places, that water will sink up to

2000 meters to where deep currents flow. A complete circuit of a deep current may take

up to 1000 years. 

Even still, deep currents are critical to the movement of nutrients around the world.

Many fisheries, for example, depend on cyclical upwelling of nutrient-rich water moving from

deep currents into local surface currents. 

While nutrients released through decomposition near the ocean floor are pulled up by upwelling,

oxygen cycles down from the surface to the deep, which keeps those decomposers and other

deep-sea organisms supplied with oxygen for respiration.

So the broad global circulation of deep currents is like a vast conveyor belt of ocean water

that brings warmth from the equator to the poles, nutrients from the floor to the surface,

and oxygen from the surface to the floor. 

Marine habitats near upwellings only cover about 1% of Earth's oceans, but account

for up to 50% of the global fish harvest. At least a billion people rely on fish for

their primary protein, so deep ocean circulation not only moves energy around the globe, but

also helps create the conditions that feed a large part of the world. 

Higher up, dominant winds and surface currents have helped move people around the globe for

thousands of years. 

With the movement of ships, has come the movement of people and the things they deem most important.

We can understand the material culture of a people by the marine debris they create. 

Some of that trash will get swept into regional surface currents like gyres, but some will

get caught by smaller local currents and wash up on shore without traveling the world.

Like there have been outbreaks of whole toys washing up on beaches, from rubber ducks to

LEGO dragons to Garfield phones. What do all these things have in common? Well, like you've

probably intuited, marine debris in the 21st century is mostly plastic. 

There are 8 million metric tons of plastic bits and debris we don't know the origin

of, or nonpoint source pollution, that's estimated to be in the oceans, but there's

also bigger garbage out there too. 

Take that whole LEGO dragon -- it didn't travel far. It came from a wrecked shipping container

that fell into the ocean after a huge once-in-a-100-years wave hit the cargo ship that was carrying it.

In fact, there are thousands of shipping containers each year that fall off cargo ships due to

rough weather or other mishaps. This map shows the movement of the 50,000 ships each day

moving goods around the globe.

Some estimates say 90% of global trade involves container ships crossing