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How do oceans circulate?

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Exploring our Oceans

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Ocean circulation plays a huge role in cycling vital nutrients within the seas and helps us transport goods on ships across the globe. Crash Course takes a closer look at how the oceans circulate by following the life of a discarded water bottle as it gets snagged in the North Pacific Garbage Patch.

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The global ocean circulation doesn’t only move water. It also determines the global climate. Without the Gulf Stream, for example, Europe’s climate wouldn’t be as mild. Besides, ocean currents redistribute oxygen and nutrients and other compounds. This doesn’t only happen horizontally but also vertically through upwelling and downwelling. Thus the thermohaline circulation ensures homogenous oxygenation and forms the physical basis for much of ocean primary production.

It is not surprising then that a weakening or even loss of some ocean currents would have catastrophic consequences. But this is precisely what some scientists are predicting as a consequence of anthropogenic climate change. Melting ice at the poles combined with rising temperatures could lead to a reduction in seawater density at the poles, which drives the thermohaline circulation. In particular, the focus has been the Atlantic Meridional Overturning Circulation, which is predicted by some to collapse by the end of the century. It is one of the main tipping points considered by the Intergovernmental Panel on Climate Change and was dramatically thematized in Roland Emmerich’s blockbuster The Day After Tomorrow.

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About Exploring our Oceans

Exploring our Oceans offers insight into the scientific marvels of the marine world, and the part you can play in uncovering the ocean's mysteries and safeguarding its future. From biology to physics to engineering, understanding our oceans involves a multitude of scientific approaches. Dive into our curated videos and supporting lesson materials, and find out how you can be a part of it all.

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  • Video created by CrashCourse
  • Lesson Plan created by Luka Seamus Wright

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