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Channelling of high-latitude boundary-layer flow

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Fig. 1.������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������� Study domain and locations of interest for this study
Fig. 2. Geographical conditions around Cape Dorset and Iqaluit. At each location, the solid arrow indicates the position of the wind sensor.Both ends of the cross-channel dashed arrows are at the same elevation as indicated
Fig. 3. Joint normalised occurrence of actual and geostrophic sur-face wind directions (total occurrence within the data period, di-vided by the occurrence of the most frequent combination of actualand geostrophic wind directions)at (a) Cape Dorset, and (b) Iqaluit.The white line connects the most frequently occurring wind direc-tions for each geostrophic wind direction.
Fig. 4. Joint normalised occurrence of surface geostrophic wind di-rections and actual wind directions at ridge-top level (600 mASL)at Iqaluit
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