mild
The North Atlantic Current brings much warmer weather to Europe. This explains why Europe is some 15˚F warmer than areas of the same latitude.
The North Atlantic Drift, a current of warm water from the tropics, flows near Europe's west coast. The prevailing westerlies, which blow west to east, pick up warmth from this current and carry it over Europe. They also carry moisture, giving the region adequate rainfall.
The North Atlantic Drift is a warm ocean current that is very powerful and important. It stretches from Florida to north-western Europe. As the warm waters of the drift flow toward western Europe it moderates the climate of that area. This allows for winters that are less cold than would be expected at that particular latitude. Without the North Atlantic Drift, many places in Europe and the United Kingdom would be as cold as Canada.
gulf stream
Europe
the north Atlantic current brings warm air to Europe
The Gulf Stream, originating in the Gulf of Mexico, passing the US east coast, crossing the Atlantic in a northwesterly direction is responsible for the temperate climate of coastal northern Europe.
The North Atlantic drift is the Gulf Stream, the most important ocean current in the Northern Hemisphere. It stretches from Florida to North Western Europe. The warm waters are effective in moderating the climate of North Western Europe
The Northern Atlantic drift is a warm ocean current in the northern part of the Atlantic Ocean that influences the climate in Europe. In Europe, the drift moves warmer waters from farther west up towards northern Europe, where it helps to warm up colder air masses from the north and results in parts of Europe being warmer than they should be.
Westerly winds bring mild, humid air from the North Atlantic Drift current, which itself is fed by the warm waters of the Gulf Stream.
The North Atlantic Drift, a current of warm water from the tropics, flows near Europe's west coast. The prevailing westerlies pick up warmth from this current and carry it over Europe. They also carry moisture, giving the region adequate rainfall.
because of the North Atlantic Drift.
the north atlantic drift.
The North Atlantic Drift
The Northern Atlantic drift is a warm ocean current in the northern part of the atlantic ocean that influences the climate in Europe. In Europe, the drift moves warmer waters from farther west up towards northern Europe, where it helps to warm up colder air masses from the north and results in parts of Europe being warmer than they should be.
The Gulf Stream dominates the climate of Northern Europe. After it travels past Canada, the current moves eastward across the Atlantic and then splits. One portion flows northward between Great Britain and Northern Europe, the other moves south along Europe and northern Africa.
The Arctic and North Atlantic oceans are two factors which affect the climate in European Europe. A climate controller for Europe is the jet streams.