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...

Full description

Bibliographic Details
Main Author: Ólafsson, Haraldur; Háskóli Íslands (University of Iceland), Veðurstofa Íslands (Icelandic Meteorological Office) and Rannsóknastofa í veðurfræði (Institute for Meteorological Research); haraldur@vedur.is
Format: Text
Language:English
Published: Croatian meteorological society; info@meteohmd.hr 2005
Subjects:
Online Access:http://hrcak.srce.hr/64697
http://hrcak.srce.hr/file/96969
id fthrcak:oai:hrcak.srce.hr:64697
record_format openpolar
spelling fthrcak:oai:hrcak.srce.hr:64697 2023-05-15T16:46:47+02:00 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
institution Open Polar
collection Hrčak - Portal of scientific journals of Croatia
op_collection_id fthrcak
language English
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
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
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
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
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
title QUASI-GEOSTROPHIC FLOW PAST MOUNTAINS
title_short 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_sort quasi-geostrophic flow past mountains
publisher Croatian meteorological society; info@meteohmd.hr
publishDate 2005
url http://hrcak.srce.hr/64697
http://hrcak.srce.hr/file/96969
genre Iceland
genre_facet Iceland
op_source Croatian meteorological journal (nikolic@cirus.dhz.hr); Vol.40 No.40
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.
_version_ 1766036886470524928