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cutting-off process

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cutting-off process [′kəd·iŋ ‚ȯf ‚präs·əs]
(meteorology)
A sequence of events by which a warm high or cold low, originally within the westerlies, becomes displaced either poleward (cutoff high) or equatorward (cutoff low) out of the westerly current; this process is evident at very high levels in the atmosphere, and it frequently produces, or is part of the production of, a blocking situation.


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A tongue of one of the pre-Wisconsinan glaciers may also have been involved in the cutting-off process.
 
 
 
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