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The North Atlantic Oscillation (NAO) is a weather phenomenon over the North Atlantic Ocean of fluctuations in the difference of atmospheric pressure at sea level (SLP) between the Icelandic Low and the Azores High.
English: Winter (December through March) index of the North Atlantic oscillation (NAO) based on the difference of normalized sea level pressure (SLP) between Gibraltar and SW Iceland since 1823, with loess smoothing (black, confidence interval in grey).
The Azores High also known as North Atlantic (Subtropical) High/Anticyclone or the Bermuda-Azores High, is a large subtropical semi-permanent centre of high atmospheric pressure typically found south of the Azores in the Atlantic Ocean, at the Horse latitudes. It forms one pole of the North Atlantic oscillation, the other being the Icelandic Low.
Atlantic hurricane tracking chart. A tropical cyclone tracking chart is used by those within hurricane-threatened areas to track tropical cyclones worldwide. In the north Atlantic basin, they are known as hurricane tracking charts. New tropical cyclone information is available at least every six hours in the Northern Hemisphere and at least ...
Low pressure, Two or three (possibly four) non-tropical areas of low pressure with central low pressure over the North Atlantic below 920 hPa have been reported, with a further unverified instance during the Night of the Big Wind (see above), these represent globally the lowest non-tropical large-scale synoptic values.
Water that upwells at lower, ice-free latitudes moves further northward due to Ekman transport and is committed to the upper cell. The warm water in the upper cell is responsible for the return flow to the North Atlantic, which occurs mainly around the coast of Africa [clarification needed] and through the Indonesian archipelago. Once this ...
Over 100 forecast products are issued daily. They cover the North Atlantic Ocean from the west coast of Europe to the U.S. and Canadian east coasts, and the North Pacific Ocean from the U.S. and Canadian west coast to the east coast of Asia. OPC weather forecasts and warnings for these areas primarily ensure the safety of ocean-crossing ...
The Gulf Stream separates from the US coast near Cape Hatteras (35°N, 75°W) and then travels eastwards across the North Atlantic, becoming the North Atlantic current at about 55°W. In the region between 75°W and 55°W it is subject to meanders and is frequently accompanied by eddies. The northern edge of the current is marked by a sharp ...