Modelling of surface wind in petuniabukta (Billefjorden, Svalbard)

Atmospheric boundary layer processes in Arctic fjords are strongly influenced by complex topography. The topographic effects may include channelling, drainage flows and mountain waves in particular (Láska et al. 2012). Modelling of these effects in the case of small-scale topography requires very hi...

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Main Authors: Chládová, Z. (Zuzana), Láska, K., Hošek, J. (Jiří)
Format: Other/Unknown Material
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/11104/0236707
id ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0432294
record_format openpolar
spelling ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0432294 2024-09-15T17:53:49+00:00 Modelling of surface wind in petuniabukta (Billefjorden, Svalbard) Chládová, Z. (Zuzana) Láska, K. Hošek, J. (Jiří) 2014 http://hdl.handle.net/11104/0236707 eng eng urn:isbn: 978-80-7394-463-6 http://hdl.handle.net/11104/0236707 wind atmospheric circulation wrf model wasp model Svalbard Arctic info:eu-repo/semantics/other info:eu-repo/semantics/publishedVersion 2014 ftczacademyscien 2024-08-19T05:32:59Z Atmospheric boundary layer processes in Arctic fjords are strongly influenced by complex topography. The topographic effects may include channelling, drainage flows and mountain waves in particular (Láska et al. 2012). Modelling of these effects in the case of small-scale topography requires very high resolution of both wind measurements and suitable tool for parameterisation of the atmospheric boundary layer. There are only few studies which deal with comparison of the observed and estimated wind conditions in the Arctic summer. In this study, the numerical simulation by means of the Weather Research Forecasting (WRF) model (Skamarock et al. 2007) and WAsP Engineering model (Troen and Petersen, 1989) were used. The WRF model can catch a large spatial variation in near-surface variables over fjords. The simulations have previously been evaluated against measurement of the weather stations on Greenland, Svalbard and Arctic Ocean in spring and the results were satisfactory. WAsP Engineering model supports mainly the estimation of loads on wind turbines and other civil engineering structures situated in moderately complex terrain. Other/Unknown Material Arctic Ocean Billefjorden Greenland Svalbard The Czech Academy of Sciences: Publication Activity (ASEP)
institution Open Polar
collection The Czech Academy of Sciences: Publication Activity (ASEP)
op_collection_id ftczacademyscien
language English
topic wind
atmospheric circulation
wrf model
wasp model
Svalbard
Arctic
spellingShingle wind
atmospheric circulation
wrf model
wasp model
Svalbard
Arctic
Chládová, Z. (Zuzana)
Láska, K.
Hošek, J. (Jiří)
Modelling of surface wind in petuniabukta (Billefjorden, Svalbard)
topic_facet wind
atmospheric circulation
wrf model
wasp model
Svalbard
Arctic
description Atmospheric boundary layer processes in Arctic fjords are strongly influenced by complex topography. The topographic effects may include channelling, drainage flows and mountain waves in particular (Láska et al. 2012). Modelling of these effects in the case of small-scale topography requires very high resolution of both wind measurements and suitable tool for parameterisation of the atmospheric boundary layer. There are only few studies which deal with comparison of the observed and estimated wind conditions in the Arctic summer. In this study, the numerical simulation by means of the Weather Research Forecasting (WRF) model (Skamarock et al. 2007) and WAsP Engineering model (Troen and Petersen, 1989) were used. The WRF model can catch a large spatial variation in near-surface variables over fjords. The simulations have previously been evaluated against measurement of the weather stations on Greenland, Svalbard and Arctic Ocean in spring and the results were satisfactory. WAsP Engineering model supports mainly the estimation of loads on wind turbines and other civil engineering structures situated in moderately complex terrain.
format Other/Unknown Material
author Chládová, Z. (Zuzana)
Láska, K.
Hošek, J. (Jiří)
author_facet Chládová, Z. (Zuzana)
Láska, K.
Hošek, J. (Jiří)
author_sort Chládová, Z. (Zuzana)
title Modelling of surface wind in petuniabukta (Billefjorden, Svalbard)
title_short Modelling of surface wind in petuniabukta (Billefjorden, Svalbard)
title_full Modelling of surface wind in petuniabukta (Billefjorden, Svalbard)
title_fullStr Modelling of surface wind in petuniabukta (Billefjorden, Svalbard)
title_full_unstemmed Modelling of surface wind in petuniabukta (Billefjorden, Svalbard)
title_sort modelling of surface wind in petuniabukta (billefjorden, svalbard)
publishDate 2014
url http://hdl.handle.net/11104/0236707
genre Arctic Ocean
Billefjorden
Greenland
Svalbard
genre_facet Arctic Ocean
Billefjorden
Greenland
Svalbard
op_relation urn:isbn: 978-80-7394-463-6
http://hdl.handle.net/11104/0236707
_version_ 1810429910777331712