| Summary: | The mesoscale atmospheric flow response to Greenland is difficult to predict. Flow over and around Greenland is affected by (i) the large and very steep elevation change between the coastal margins and the central plateau (~3000m), (ii) the combination of very rough surfaces (roughness length zo~1-10m) and jagged mountains around the coasts, (iii) the strong katabatic flows from the plateau down to the coasts (van den Broeke and Gallee 1996), (iv) the presence of the semi-permanent Icelandic Low, and (v) air-sea-ice interaction processes (Scorer 1988). Previously curated at: http://cedadocs.ceda.ac.uk/173/ The publish date on this item was its original published date. Main files in this record: UCL.Mesoscale_modelling_of_flow_response_to_Greenland.pdf Item originally deposited with Centre for Environmental Data Analysis (CEDA) document repository by Ms Belinda Robinson. Transferred to CEDA document repository community on Zenodo on 2022-11-24
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