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Icelandic low

   Also found in: Wikipedia 0.01 sec.
Icelandic low [′īs′land·ik ′lō]
(meteorology)
The low-pressure center located near Iceland (mainly between Iceland and southern Greenland) on mean charts of sea-level pressure.
On a synoptic chart, any low centered near Iceland.


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The weather in Scotland is highly influenced by a semi-permanent pressure system called the Icelandic Low, and that in Morocco by another called the Azores High.
When the NAO is in its low state, the Icelandic low pressure center is displaced far to the south, off Newfoundland, and there is a high pressure center over northern Greenland, causing cold dry polar air to blow across northern Europe, and then westward across the northern subpolar area towards North America, warming on the way by the heat liberated from the ocean to the overlying atmosphere.
 
 
 
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