North Atlantic Drift

The North Atlantic Drift is a powerful ocean current that transports warm water from the Gulf of Mexico across the Atlantic Ocean toward Europe. It is an extension of the Gulf Stream and helps moderate the climate of Western Europe, making it milder than other regions at similar latitudes. By carrying warm water northeastward, the drift influences weather patterns, contributing to warmer winters and a more stable climate in countries like the UK, Ireland, and Scandinavia. Essentially, it acts as a natural conveyor belt, redistributing heat from the tropics to higher latitudes.