Gulf Stream - Properties

Properties

The Gulf Stream proper is a western-intensified current, driven largely by wind stress. The North Atlantic Drift, in contrast, is largely thermohaline circulation-driven. By carrying warm water northeast across the Atlantic, it makes Western and especially Northern Europe warmer than it otherwise would be. However, the extent of its contribution to the actual temperature differential between North America and Europe is a matter of dispute as there is a recent minority opinion within the science community that this temperature difference is mainly due to the Atlantic Ocean being upwind of western Europe (producing an oceanic climate) and a landmass being upwind of the east coast of North America.

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