Aleutian low: Difference between revisions

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The low pressure center located near the Aleutian Islands on mean charts of [[sea level pressure|sea level  pressure]].<br/> It represents one of the main centers of action in the atmospheric [[circulation]] of the Northern  Hemisphere. The Aleutian low is most intense in the winter months; in summer it is displaced  toward the North Pole and is almost nonexistent. On a daily basis, the area of the Aleutian low  is marked by alternating high and low pressure centers, moving generally to the eastward; it is not  the scene of an intense stationary [[low]]. Normally the depth of [[intensity]] of the low pressure areas  exceeds the [[intensity]] of the high pressure areas, so that the region is one of low pressure on the  average. The travelling cyclones of subpolar latitudes usually reach maximum [[intensity]] in the area  of the Aleutian low. The Aleutian low and its counterpart in the Atlantic Ocean, the [[Icelandic low|Icelandic  low]], compose the Northern Hemisphere's [[subpolar low pressure belt]].
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== Aleutian low ==
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<div class="definition"><div class="short_definition">The low pressure center located near the Aleutian Islands on mean charts of [[sea level  pressure]].</div><br/> <div class="paragraph">It represents one of the main centers of action in the atmospheric [[circulation]] of the Northern  Hemisphere. The Aleutian low is most intense in the winter months; in summer it is displaced  toward the North Pole and is almost nonexistent. On a daily basis, the area of the Aleutian low  is marked by alternating high and low pressure centers, moving generally to the eastward; it is not  the scene of an intense stationary [[low]]. Normally the depth of [[intensity]] of the low pressure areas  exceeds the [[intensity]] of the high pressure areas, so that the region is one of low pressure on the  average. The travelling cyclones of subpolar latitudes usually reach maximum [[intensity]] in the area  of the Aleutian low. The Aleutian low and its counterpart in the Atlantic Ocean, the [[Icelandic  low]], compose the Northern Hemisphere's [[subpolar low pressure belt]].</div><br/> </div>
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Latest revision as of 16:23, 7 November 2023

The low pressure center located near the Aleutian Islands on mean charts of sea level pressure.
It represents one of the main centers of action in the atmospheric circulation of the Northern Hemisphere. The Aleutian low is most intense in the winter months; in summer it is displaced toward the North Pole and is almost nonexistent. On a daily basis, the area of the Aleutian low is marked by alternating high and low pressure centers, moving generally to the eastward; it is not the scene of an intense stationary low. Normally the depth of intensity of the low pressure areas exceeds the intensity of the high pressure areas, so that the region is one of low pressure on the average. The travelling cyclones of subpolar latitudes usually reach maximum intensity in the area of the Aleutian low. The Aleutian low and its counterpart in the Atlantic Ocean, the Icelandic low, compose the Northern Hemisphere's subpolar low pressure belt.


The low pressure center located near the Aleutian Islands on mean charts of sea level pressure.
It represents one of the main centers of action in the atmospheric circulation of the Northern Hemisphere. The Aleutian low is most intense in the winter months; in summer it is displaced toward the North Pole and is almost nonexistent. On a daily basis, the area of the Aleutian low is marked by alternating high and low pressure centers, moving generally to the eastward; it is not the scene of an intense stationary low. Normally the depth of intensity of the low pressure areas exceeds the intensity of the high pressure areas, so that the region is one of low pressure on the average. The travelling cyclones of subpolar latitudes usually reach maximum intensity in the area of the Aleutian low. The Aleutian low and its counterpart in the Atlantic Ocean, the Icelandic low, compose the Northern Hemisphere's subpolar low pressure belt.

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