QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS
Abstract: Blocked flow at moderate Rossby numbers is studied and an analytic expression is derived for the vertical velocities on each side of the wake: W = (Uo h) / (f Lx Ly) Where Uo is the incoming wind speed, h is the mountain height, f is Coriolis parameter, Ly is mountain half-width and Ly is...
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Format: | Text |
Language: | English |
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Croatian meteorological society; info@meteohmd.hr
2005
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Online Access: | http://hrcak.srce.hr/64697 http://hrcak.srce.hr/file/96969 |
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author | Ólafsson, Haraldur; Háskóli Íslands (University of Iceland), Veðurstofa Íslands (Icelandic Meteorological Office) and Rannsóknastofa í veðurfræði (Institute for Meteorological Research); haraldur@vedur.is |
author_facet | Ólafsson, Haraldur; Háskóli Íslands (University of Iceland), Veðurstofa Íslands (Icelandic Meteorological Office) and Rannsóknastofa í veðurfræði (Institute for Meteorological Research); haraldur@vedur.is |
author_sort | Ólafsson, Haraldur; Háskóli Íslands (University of Iceland), Veðurstofa Íslands (Icelandic Meteorological Office) and Rannsóknastofa í veðurfræði (Institute for Meteorological Research); haraldur@vedur.is |
collection | Hrčak - Portal of scientific journals of Croatia |
description | Abstract: Blocked flow at moderate Rossby numbers is studied and an analytic expression is derived for the vertical velocities on each side of the wake: W = (Uo h) / (f Lx Ly) Where Uo is the incoming wind speed, h is the mountain height, f is Coriolis parameter, Ly is mountain half-width and Ly is a length scale of the vertical mortion downstream of the edges of the mountains. To illustrate the use of the above expression, a collection of flows over Iceland is presented and the calculated vertical velocities are compared to the number of days with precipitation in two different regions. |
format | Text |
genre | Iceland |
genre_facet | Iceland |
id | fthrcak:oai:hrcak.srce.hr:64697 |
institution | Open Polar |
language | English |
op_collection_id | fthrcak |
op_relation | http://hrcak.srce.hr/64697 http://hrcak.srce.hr/file/96969 |
op_rights | The papers of this Journal are free of charge for personal or educational use, with respect of copyright of authors and publisher. |
op_source | Croatian meteorological journal (nikolic@cirus.dhz.hr); Vol.40 No.40 |
publishDate | 2005 |
publisher | Croatian meteorological society; info@meteohmd.hr |
record_format | openpolar |
spelling | fthrcak:oai:hrcak.srce.hr:64697 2025-01-16T22:32:52+00:00 QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS Ólafsson, Haraldur; Háskóli Íslands (University of Iceland), Veðurstofa Íslands (Icelandic Meteorological Office) and Rannsóknastofa í veðurfræði (Institute for Meteorological Research); haraldur@vedur.is 2005-12-15 pdf http://hrcak.srce.hr/64697 http://hrcak.srce.hr/file/96969 en eng Croatian meteorological society; info@meteohmd.hr http://hrcak.srce.hr/64697 http://hrcak.srce.hr/file/96969 The papers of this Journal are free of charge for personal or educational use, with respect of copyright of authors and publisher. Croatian meteorological journal (nikolic@cirus.dhz.hr); Vol.40 No.40 quasi-geostrophic flow;Rossby number;Froude number;Nh/U;non-dimensional mountain height;asymetric ascending motion;Iceland Coriolis force;blocking;conceptual model;wake;corner winds text 2005 fthrcak 2012-10-27T15:58:16Z Abstract: Blocked flow at moderate Rossby numbers is studied and an analytic expression is derived for the vertical velocities on each side of the wake: W = (Uo h) / (f Lx Ly) Where Uo is the incoming wind speed, h is the mountain height, f is Coriolis parameter, Ly is mountain half-width and Ly is a length scale of the vertical mortion downstream of the edges of the mountains. To illustrate the use of the above expression, a collection of flows over Iceland is presented and the calculated vertical velocities are compared to the number of days with precipitation in two different regions. Text Iceland Hrčak - Portal of scientific journals of Croatia |
spellingShingle | quasi-geostrophic flow;Rossby number;Froude number;Nh/U;non-dimensional mountain height;asymetric ascending motion;Iceland Coriolis force;blocking;conceptual model;wake;corner winds Ólafsson, Haraldur; Háskóli Íslands (University of Iceland), Veðurstofa Íslands (Icelandic Meteorological Office) and Rannsóknastofa í veðurfræði (Institute for Meteorological Research); haraldur@vedur.is QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS |
title | QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS |
title_full | QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS |
title_fullStr | QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS |
title_full_unstemmed | QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS |
title_short | QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS |
title_sort | quasi-geostrophic flow past mountains |
topic | quasi-geostrophic flow;Rossby number;Froude number;Nh/U;non-dimensional mountain height;asymetric ascending motion;Iceland Coriolis force;blocking;conceptual model;wake;corner winds |
topic_facet | quasi-geostrophic flow;Rossby number;Froude number;Nh/U;non-dimensional mountain height;asymetric ascending motion;Iceland Coriolis force;blocking;conceptual model;wake;corner winds |
url | http://hrcak.srce.hr/64697 http://hrcak.srce.hr/file/96969 |