Influence of different wind directions in relation to topography on the outbreak of convection in Northern England

The influence of different wind directions on the outbreak of convection in Northern England, was investigated with a high-resolution numerical model. The Clark model, a 3D finite-difference, non-hydrostatic model was used in this study. It was initialised with the topography of Northern England...

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Main Authors: J. Thielen, A. Gadian
Format: Article
Language:English
Published: Copernicus Publications 1996-10-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/14/1078/1996/angeo-14-1078-1996.pdf
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author J. Thielen
A. Gadian
author_facet J. Thielen
A. Gadian
author_sort J. Thielen
collection DOAJ
description The influence of different wind directions on the outbreak of convection in Northern England, was investigated with a high-resolution numerical model. The Clark model, a 3D finite-difference, non-hydrostatic model was used in this study. It was initialised with the topography of Northern England, a representation of surface characteristics, and used a routinely available meteorological sounding, typical of the unstable conditions. Results showed that convective cells were initially triggered in the lee of the elevated terrain, and that only after the convection had developed, were cells upwind of the elevated terrain produced. The windward slopes themselves seemed sheltered from convection. Under most wind directions, the central Pennines (the Forest of Trawden and the Forest of Rossendale) seemed particularly affected by convective rainfall.
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spelling doaj.art-663fcfd422214e248dc2f291ba17767f2022-12-21T18:28:04ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761996-10-01141078108710.1007/s00585-996-1078-3Influence of different wind directions in relation to topography on the outbreak of convection in Northern EnglandJ. Thielen0A. Gadian1L.T.H.E., F-38041 Grenoble Cedex 09, FranceDepartment of Physics, UMIST, Manchester M60 1QD, UKThe influence of different wind directions on the outbreak of convection in Northern England, was investigated with a high-resolution numerical model. The Clark model, a 3D finite-difference, non-hydrostatic model was used in this study. It was initialised with the topography of Northern England, a representation of surface characteristics, and used a routinely available meteorological sounding, typical of the unstable conditions. Results showed that convective cells were initially triggered in the lee of the elevated terrain, and that only after the convection had developed, were cells upwind of the elevated terrain produced. The windward slopes themselves seemed sheltered from convection. Under most wind directions, the central Pennines (the Forest of Trawden and the Forest of Rossendale) seemed particularly affected by convective rainfall.https://www.ann-geophys.net/14/1078/1996/angeo-14-1078-1996.pdf
spellingShingle J. Thielen
A. Gadian
Influence of different wind directions in relation to topography on the outbreak of convection in Northern England
Annales Geophysicae
title Influence of different wind directions in relation to topography on the outbreak of convection in Northern England
title_full Influence of different wind directions in relation to topography on the outbreak of convection in Northern England
title_fullStr Influence of different wind directions in relation to topography on the outbreak of convection in Northern England
title_full_unstemmed Influence of different wind directions in relation to topography on the outbreak of convection in Northern England
title_short Influence of different wind directions in relation to topography on the outbreak of convection in Northern England
title_sort influence of different wind directions in relation to topography on the outbreak of convection in northern england
url https://www.ann-geophys.net/14/1078/1996/angeo-14-1078-1996.pdf
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AT agadian influenceofdifferentwinddirectionsinrelationtotopographyontheoutbreakofconvectioninnorthernengland