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periglacial climate

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periglacial climate [¦per·ə′glā·shəl ′klī·mət]
(climatology)
The climate which is characteristic of the regions immediately bordering the outer perimeter of an ice cap or continental glacier; the principal climatic feature is the high frequency of very cold and dry winds off the ice area; it is also thought that these regions offer ideal conditions for the maintenance of a belt of intense cyclonic activity.


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Landforms, ice wedge polygons, and published reports on diatoms, insects, palynomorphs, plant and vertebrate fossils record the transition from glacial to periglacial climate to the Bolling-Allerod warming in Northern Oakland County.
 
 
 
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