Mesoscale Modelling of flow response to Greenland
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~1-1...
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ftzenodo:oai:zenodo.org:7354254 2024-09-15T18:08:48+00:00 Mesoscale Modelling of flow response to Greenland Orr, Andrew Hunt, Julian University College London, United Kingdom 2002-01-01 https://doi.org/10.5281/zenodo.7354254 eng eng Zenodo https://zenodo.org/communities/ceda-document-repository https://doi.org/10.5281/zenodo.7354253 https://doi.org/10.5281/zenodo.7354254 oai:zenodo.org:7354254 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/workingPaper 2002 ftzenodo https://doi.org/10.5281/zenodo.735425410.5281/zenodo.7354253 2024-07-26T14:00:28Z 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 Report Greenland Sea ice Zenodo |
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English |
description |
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 |
author2 |
University College London, United Kingdom |
format |
Report |
author |
Orr, Andrew Hunt, Julian |
spellingShingle |
Orr, Andrew Hunt, Julian Mesoscale Modelling of flow response to Greenland |
author_facet |
Orr, Andrew Hunt, Julian |
author_sort |
Orr, Andrew |
title |
Mesoscale Modelling of flow response to Greenland |
title_short |
Mesoscale Modelling of flow response to Greenland |
title_full |
Mesoscale Modelling of flow response to Greenland |
title_fullStr |
Mesoscale Modelling of flow response to Greenland |
title_full_unstemmed |
Mesoscale Modelling of flow response to Greenland |
title_sort |
mesoscale modelling of flow response to greenland |
publisher |
Zenodo |
publishDate |
2002 |
url |
https://doi.org/10.5281/zenodo.7354254 |
genre |
Greenland Sea ice |
genre_facet |
Greenland Sea ice |
op_relation |
https://zenodo.org/communities/ceda-document-repository https://doi.org/10.5281/zenodo.7354253 https://doi.org/10.5281/zenodo.7354254 oai:zenodo.org:7354254 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.735425410.5281/zenodo.7354253 |
_version_ |
1810446179825090560 |