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Climate is influenced by the temperatures of the surface waters and water currents as well as winds. Because of the ocean's great capacity to store
and release heat, maritime climates are more moderate and have less extreme seasonal variations than inland climates. Precipitation can be
approximated from coastal weather data and air temperature from water temperatures.
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The Gulf Stream and its northern extension towards Europe, the North Atlantic Drift, for example, warms the atmosphere of the British Isles and
north-western Europe and influences we
ather and climate as far south as the no
rthern Mediterranean. The cold water currents contribute to heavy fog off the
coast of eastern Canada (
the Grand Banks of Newfoundland area) and Africa's north-western coast. In general, winds transport moisture and air over land areas. Hurricanes
develop in the s
outhern part of the North Atlantic Ocean. More local particular weather examples could be found in
examples such as the; Azores High, Benguela Current, Nor'easter.t salinity values ar<img src="http://www.derkey.co/1c8a25e378e456f8687cc034f026_071b0754-010102010001/V/" alt=" ">
The oceans are the major source of the atmospheric moisture that i
s obtained through evaporation. Climatic zones vary with latitude; the warmest zones stretch across the Atlantic north of the equator. The
coldest zones are in high latitudes, with the coldest regions corresponding to the areas covered by sea ice. Ocean currents influence climate by
transporting warm and cold waters to other regions. Th
e winds that are cooled or warmed when blowing over these currents influence adjacent land areas.
th low rainfall and high evaporation.<img src="http://www.derkey.co/1c8a25e378e456f8687cc034f026_071b0754-010102010001/V/" alt=" ">
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