The Major Ocean Currents of the World
In 1992, a cargo ship carrying rubber ducks got caught in a storm. The ocean currents swept away 28,000 of them.
Where did they go? They didn’t stick together. Instead they ended up all over the world.
This story tells us that ocean currents aren’t easy to follow. Their paths are dynamic.
For example, NASA’s Scientific Visual Studio ocean currents maps shows the beauty and complex nature of this phenomenon.
Ahoy, matey! Let’s set sail on a journey to Earth’s major ocean currents.
A deep dive into the world’s major ocean currents
If you look at a world map, you can see that Earth’s 5 oceans are vast. In fact, they cover more than 70% of Earth.
Water is always on the move. Ocean currents are like giant conveyor belts flowing through the oceans moving huge amounts of water all the time.
From cold to hot (and vice versa), oceans transport water like a giant conveyor belt. The major ocean currents roughly follow a common set of circular paths.
While wind drives surface ocean currents from the Coriolis effect, temperature and salt gradients mostly influences deep ocean currents.
What are the names of the major ocean currents in the world?
But we can still divide them into major ocean currents that circulate water in our 5 oceans:
|Gulf Stream||Warm ocean current originating in Gulf of Mexico along the east coast of the United States|
|Labrador Current||Cold ocean current flowing from the Arctic Ocean south along the east coast of Canada|
|North Equatorial Current||East-to-west flowing current from 10°-20°N in the Pacific and Atlantic Ocean|
|North Equatorial Counter Current (NECC)||West-to-east flowing current from 3°-10°N in the Atlantic, Indian Ocean and Pacific Ocean|
|South Equatorial Current||East-to-west current flowing between the equator and about 20°S in the Pacific, Atlantic, and Indian Ocean|
|South Equatorial Counter Current (SECC)||Weak east-flowing current near 8°S in the Atlantic and Pacific Ocean|
|Kuroshio Current||North-flowing warm current off the coast of Japan in the Pacific Ocean|
|Alaska Current||Southwestern warm water current off the coast of Alaska and west coast of Canada.|
|California Current||Southward flowing current off the west coast of the United States in the Pacific Ocean|
How are warm and cold currents different?
The wind and sun make ocean currents move. At the equator, the sun is strongest heating water the most there. When water heats, water molecules vibrate faster and eventually move farther apart.
From the equator, hot water pushes outward to north and south pole south pole. At the same time, cold water from the north and south poles collide with this warm water.
Because Earth spins on its axis, water flows in a circular pattern. For example, oceans in the northern hemisphere move mostly clockwise. But in the southern hemisphere, ocean currents move mostly counter-clockwise.
For example, the Gulf stream current pushes warm air to Europe. It flows around the Atlantic Ocean like a clock. Because of the Gulf stream, this is why parts of Europe has such a temperate climate.
Ocean water can hold more heat than air. For example, thermohaline currents (thermo = temperature, haline = salt) with warm, salt water sinking and rising. Salty water pushes not so salty water away. We get a current. Winds can also make ocean currents.
Which satellites track ocean movement and currents?
We don’t know much about what’s under our oceans. In fact, 80% of oceans are unexplored. Satellites can’t see inside the oceans. Instead, satellites like GRACE and GOCE measure gravity to map out oceanic topography.
Satellites also track ocean movement and currents. For example, NASA satellites like Poseidon and Jason have been observing ocean currents from space. These satellites monitor ocean motion by measuring sea surface height.
Overall, satellites cover more ground for tracking ocean currents. NASA/JPL’s perpetual ocean visualizes the slow-moving, swirling pools called ocean eddies.
What technology measures deep ocean currents?
There are other types of technology that map out our oceans. For examples, here are some examples of technology used for ocean exploration:
- Marker buoys
- Underwater robots
Self-locating datum marker buoys monitor currents by sending out a radio signal. By monitoring these signals, we can follow and see where ocean currents are flowing. But we need a lot of them to get the whole picture.
Alternatively, fleet of underwater robots or “Argo” research deep ocean currents. For example, Argo research vessels conduct research on ocean heat and our changing oceans.
Why do oceans have salt?
What makes oceans different from freshwater is that they contain salt and minerals. This is because heat from the sun evaporates water. When water evaporates, salt remains in the ocean.
The water vapor rises into the sky, cools and forms clouds. Then, it falls down as rain again. When rain water falls on the land, it washes minerals and salt from the soil into lakes and rivers. But they don’t stay there.
They float downhill to an outlet at the nearest ocean. So, lakes and rivers constantly have the minerals washed away. Oceans are salty because runoff transports minerals and salts from the surface.
With the exception of the Great Salt Lake which doesn’t have an outlet. Salt built up in the Great Salt Lake until its 4 times greater than oceans.
When ocean evaporates from heat, salt remains in the ocean and water rises. So, unlike salty oceans, lakes and rivers constantly have the minerals washed away.
What living things rely on ocean currents?
Fish rely on moving water for food and oxygen. That’s why aquariums have artificial currents moving water.
And living things need ocean currents for food, climate and transportation
Wind and salt keep ocean water moving.
For example, our ocean’s motion significantly affects Earth’s weather and climate.
READ MORE: 10 Unbelievable Weather and Climate Facts
1. TED Ed Lesson – How Ocean Currents Work
This TED-Ed lesson features how ocean currents work. It starts with a story of how rubber ducks got swept away by ocean currents.
Then, it gets into what influences ocean currents. For example, the wind, tides, water density, rotation and even ocean floor topography influences currents in the oceans.
Finally, the lesson contrasts the differences between surface and deep ocean currents. For example, surface currents control the motion of about 10% of the upper ocean space. Then, deep ocean currents occupy the other 90%.
2. NASA’s Scientific Visual Studio: Perceptual Ocean
As you’ve learned, wind, density and variety of forces drive ocean currents. But how does this all look in the big picture?
NASA’s Scientific Visual Studio uses ocean flow data from satellite (Topex/Poseidon, Jason-1/2, QuikScat and GRACE) and in-situ data. The result?
A visceral experience known as the perceptual ocean map spanning hundreds of thousands of kilometers of our ocean surface.