1887

oa Madoqua - The influence of a synoptic scale disturbance on topographically induced boundary layer circulations over the central Namib Desert

 

Abstract

Local climates of coastal areas are characterised by the modification of synoptic-scale airflow by thermally and topographically induced diurnal oscillations of the lower boundary layer.

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/content/madoqua/18/2/AJA10115498_375
1993-01-01
2016-12-09
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