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The North Atlantic Drift is an ocean current that carries warm water across the Atlantic Ocean. The water warms the air above it, and wind carries that air over land. It has a huge impact on the climates of Europe and keeps the continent warmer than other regions at the same latitude. A great example of how the North Atlantic Drift affects Europe's climate can be seen when comparing Glasgow, Scotland, to Moscow, Russia. Both locations are at similar latitudes: Glasgow is located at 55°87'0" N, and Moscow is located at 55°45'0" N. Glasgow is considered a marine west coast climate, with warm summers and mild winters. The temperature difference between winter and summer is only about 50°. Moscow, though at the same latitude, has a very different climate. Moscow is a humid continental climate, which means it has hot summers and cold winters. The region has four distinct seasons and extreme temperature changes from winter to summer, with a difference of over 100°. These differences are attributed to the North Atlantic Drift instead of latitude. Scotland is affected by the warm ocean currents because of its location near the ocean. Moscow is farther inland, so it does not receive the same benefit as those areas closer to the water.
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