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North Atlantic Current

Adapted from Wikipedia · Discoverer experience

Powerful ocean waves crashing along the California coastline during a stormy day.

The North Atlantic Current (NAC), also known as North Atlantic Drift and North Atlantic Sea Movement, is a powerful warm western boundary current within the Atlantic Ocean. It extends the Gulf Stream northeastward, playing an important role in shaping the climate of regions it passes through.

This current helps carry warm water from the tropics toward higher latitudes, influencing weather patterns and creating milder climates in areas such as northwestern Europe. Because it moves warm water northward, it helps keep places like the United Kingdom and Norway much warmer than other regions at similar latitudes.

The North Atlantic Current is part of a larger system of ocean currents that helps regulate Earth’s climate by distributing heat around the planet. Its strength and path can change over time, affecting both marine life and human activities such as fishing and shipping.

Characteristics

The North Atlantic Current starts where the Gulf Stream turns north near a deep underwater ridge called the Southeast Newfoundland Rise, close to the Grand Banks of Newfoundland. It flows north along the east side of the Grand Banks before turning east across the Atlantic Ocean. This current carries a lot of warm water from tropical areas to colder northern parts.

As it moves, the North Atlantic Current changes direction based on underwater landforms. Near the Mid-Atlantic Ridge, it splits into different branches. One branch flows southeast and becomes the Canary Current near Africa, while another continues north along the coast of Northwestern Europe. The current is part of a large system of ocean movements that helps move warm water around the globe, affecting climates, especially in Europe.

Climate change

See also: Tipping points in the climate system

Modelled 21st century warming under the "intermediate" climate change scenario (top). The potential collapse of the subpolar gyre in this scenario (middle). The collapse of the entire AMOC (bottom).

Some studies suggest that parts of the ocean currents in the North Atlantic could change if the Earth gets warmer. This might cause cooler temperatures in places like Western Europe and the East Coast of the United States.

A few models show that these changes could happen if global warming reaches certain levels, but the exact timing and effects are still being studied. Scientists are carefully watching these patterns to understand how they might affect weather and climate in the future.

Images

A close-up of Aegopodium podagraria leaves, commonly known as ground elder, displayed against a black background.

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This article is a child-friendly adaptation of the Wikipedia article on North Atlantic Current, available under CC BY-SA 4.0.

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