Science Facts

What Drives Ocean Currents? – Full Working Process

Ocean Currents Circulation

The oceans cover two-thirds of the Earth’s surface. That’s hundreds of times heavier than the entire atmosphere. Earth’s oceans are connected by a vast, global conveyor belt of moving water. A planetary circulatory system that transports heat, nutrients, and even animals around the globe. And this circulatory system keeps us alive. Earth’s network of moving ocean water keeps the planet healthy.

It powers a huge part of Earth’s weather and climate and shapes whole ecosystems. Ocean currents have even influenced the history of human civilization. And the engine of this whole global ocean current? It’s powered by just salt, some sunlight, and a little wind.

What drives ocean currents?

Oceans ocean currents form due to cold water close to the surface sinking and swapping places with warmer water. This cyclical motion causes vertical currents. It is air which moving all that water around ocean currents. The oceans aren’t separate things. They’re tied together by a huge ocean current which is the ocean conveyor.

The conveyor belt is a long-moving loop of ocean currents that drives water, nutrients, plants, and animals worldwide. It is a mixture of warm shallow currents at the surface with colder, deeper currents underneath. It drives huge amounts of water, and some sections have a current of around 10 Sverdrups. Sverdrup is the special unit that ocean scientists use to talk about the vast quantities of water going round in the oceans.

  • One Sverdrup is a current of 1 million cubic meters passing by per second!

The circulation is also huge in terms of time. It can take one bit of water a thousand years to make one loop around the swirling global path. So what makes this huge conveyer run?

The first thing you need to know about how ocean currents work is. There are lots of ways that ocean currents work. Near the surface, ocean currents are controlled mainly through the wind. Just like blowing across the top of water pulls the water along with it. Surface currents are influenced by tides, the rotation of the Earth, even the shape of the land. But more than 9/10ths of the ocean’s water is pulled by a deeper force: density.

  • Hot water is less dense than cold water. Because its molecules are a bit farther apart, you can’t fit as much water in the same volume. So a volume of hot water weighs a little bit less than the same volume of cold water. And cold water sinks below the warmer water.
  • The blue water is much much colder than the red water. Just like cold ocean water, the layer of cold water sink beneath the red, warm water. When it speeds up the force of the rising and falling water densities creating a current, it is one of the major driving forces of Earth’s deep ocean circulation: colder waters sinking and warmer waters rising.

In saltwater, the dissolved salt ions fill the unused space between water molecules. It means there is more mass in a given unit of volume of saltwater compared to freshwater. So saltier water is denser than fresher water. Temperature and saltiness are crucial to how the ocean conveyor circulates.

Ocean Currents Circulation System
Ocean Currents Circulation System

What is thermohaline circulation? Thermo is referring to temperature and haline to saltiness. In high latitudes, cold water on the surface of the ocean gets saltier as water evaporates. And when sea ice forms, it pulls pure water out of the sea and leaves salt behind, making the ocean water saltier.

The heat from the sun eventually warms the cold water at the surface, where evaporation makes the water saltier. This warm salted water is carried northwards by large, powerful wind-driven ocean currents like the Gulf Stream, up the U.S. east coast, then into the North Atlantic region. Here it releases heat into the atmosphere and warms Western Europe. This water becomes very cold and dense again, sinks to the deep ocean, and the cycle continues.

The formation of cold, salty water in the north Atlantic acts as a pump, driving nearly half of Earth’s deep ocean water circulatory system. This section of the great ocean conveyor is called the Atlantic meridional overturning circulation or AMOC. The heat released by the AMOC has huge climate effects, bringing moderate rains to Europe and bringing about a million power plants-worth of heat to some parts of the planet! Consider that London in the UK is roughly the same latitude as Calgary, Canada, but Calgary is way colder! And that’s in part to the heating Europe gets from the AMOC.

How do global ocean currents drive?

The global conveyor belt is a series of ocean currents that snake around the world. They are called haline thermal currents because they are the result of changes in temperature and salinity. These changes in temperature and salinity create currents in the ocean. The conveyor belt begins on the surface of the sea near the pole in North Atlantic. The Arctic temperature chills the water. It also gets saltier because when ice forms in the ocean, the salt does not freeze and is left behind in the surrounding water.

Surface water moves in to replace the sinking water and creates a current that moves south towards the equator down towards the ends of Africa and South America. The current now travels around the edge of Antarctica, where the water cools and sinks again. As it does in the North Atlantic thus the conveyor belt gets recharged. As it moves around Antarctica, two sections split off of the conveyor and moved northward. One section moves into the Indian Ocean, the other into the Pacific Ocean.

The two branches of the current warm and rise as they travel northward, then loop back southward and westward. The non-warm surface waters continue circulating the globe. And eventually, return to the North Atlantic, where the cycle begins again. The conveyor belt moves at a much slower speed than wind has driven or tidal currents.

Importance of ocean currents drive

Ocean currents are significant. They control weather patterns around the world. Researchers have argued that a big part of Europe’s political and economic power over the last several millennia has come from the moderate climate conditions brought by the AMOC. If northern Europe was as cold as its latitude suggests, then maybe the Romans don’t Empire as far. The Vikings don’t Viking everywhere. The English, Dutch, and the Spanish would have spent more time huddling next to the fireplace instead of colonizing every country on the map.

All this has climate change that’s a pretty important ocean circulation. Climate scientists think an interruption of the AMOC in the past may have triggered a sudden, extremely cold spike in the Northern Hemisphere climate. And there’s a reason they call it global warming: pretty much everywhere is heating up.

Recent studies showed that the ocean currents in the North Atlantic are slowing down. It means that the circulation in the ocean is causing fish populations to decline sea levels to rise, and a dramatic change in global climates. Scientists hypothesized that increasing temperatures in the atmosphere and decreasing salinity in the ocean are significant factors behind this change.

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