Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field

The mesoscale circulation along the west shore of Spitsbergen is largely controlled by the difference in temperature between the glaciers and surface sea temperatures. We describe how the mesoscale effect influences the atmospheric circulation patterns. The conducted research was based on reanalysis...

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Published in:Atmosphere
Main Authors: Małgorzata Kitowska, Tomasz Petelski
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12091165
https://doaj.org/article/0e5e5cbed5264bc7887eb662fd0788b0
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spelling ftdoajarticles:oai:doaj.org/article:0e5e5cbed5264bc7887eb662fd0788b0 2023-05-15T15:07:31+02:00 Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field Małgorzata Kitowska Tomasz Petelski 2021-09-01T00:00:00Z https://doi.org/10.3390/atmos12091165 https://doaj.org/article/0e5e5cbed5264bc7887eb662fd0788b0 EN eng MDPI AG https://www.mdpi.com/2073-4433/12/9/1165 https://doaj.org/toc/2073-4433 doi:10.3390/atmos12091165 2073-4433 https://doaj.org/article/0e5e5cbed5264bc7887eb662fd0788b0 Atmosphere, Vol 12, Iss 1165, p 1165 (2021) arctic svalbard atmospheric circulation climate wind Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.3390/atmos12091165 2022-12-31T07:40:42Z The mesoscale circulation along the west shore of Spitsbergen is largely controlled by the difference in temperature between the glaciers and surface sea temperatures. We describe how the mesoscale effect influences the atmospheric circulation patterns. The conducted research was based on reanalysis data, model data, and atmospheric measurements; wind data from different sources and scales were compared and analysed. We discuss the situations wherein the mesoscale effect can be identified by analysing the wind direction or its velocity. This study shows the role of the mesoscale effect on the wind in the Svalbard region. Different situations according to the atmospheric patterns taken from a catalogue of 21 circulation types for each day created for Svalbard are analysed and compared with cases of land-sea breeze type circulation for the 20-year period between 1994 and 2013. It is proved that even if it is not possible to distinguish this mesoscale effect based on the difference between local and large-scale wind directions, this factor can be observed by studying the wind speeds. It is claimed that as long as there are glaciers on Spitsbergen, there will be a mesoscale land-sea breeze type circulation controlled by the difference in air temperature over land and water. Article in Journal/Newspaper Arctic Svalbard Spitsbergen Directory of Open Access Journals: DOAJ Articles Arctic Svalbard Atmosphere 12 9 1165
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic arctic
svalbard
atmospheric circulation
climate
wind
Meteorology. Climatology
QC851-999
spellingShingle arctic
svalbard
atmospheric circulation
climate
wind
Meteorology. Climatology
QC851-999
Małgorzata Kitowska
Tomasz Petelski
Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field
topic_facet arctic
svalbard
atmospheric circulation
climate
wind
Meteorology. Climatology
QC851-999
description The mesoscale circulation along the west shore of Spitsbergen is largely controlled by the difference in temperature between the glaciers and surface sea temperatures. We describe how the mesoscale effect influences the atmospheric circulation patterns. The conducted research was based on reanalysis data, model data, and atmospheric measurements; wind data from different sources and scales were compared and analysed. We discuss the situations wherein the mesoscale effect can be identified by analysing the wind direction or its velocity. This study shows the role of the mesoscale effect on the wind in the Svalbard region. Different situations according to the atmospheric patterns taken from a catalogue of 21 circulation types for each day created for Svalbard are analysed and compared with cases of land-sea breeze type circulation for the 20-year period between 1994 and 2013. It is proved that even if it is not possible to distinguish this mesoscale effect based on the difference between local and large-scale wind directions, this factor can be observed by studying the wind speeds. It is claimed that as long as there are glaciers on Spitsbergen, there will be a mesoscale land-sea breeze type circulation controlled by the difference in air temperature over land and water.
format Article in Journal/Newspaper
author Małgorzata Kitowska
Tomasz Petelski
author_facet Małgorzata Kitowska
Tomasz Petelski
author_sort Małgorzata Kitowska
title Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field
title_short Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field
title_full Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field
title_fullStr Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field
title_full_unstemmed Svalbard’s Mesoscale Environmental Factor Impact on the Wind Field
title_sort svalbard’s mesoscale environmental factor impact on the wind field
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/atmos12091165
https://doaj.org/article/0e5e5cbed5264bc7887eb662fd0788b0
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Svalbard
Spitsbergen
genre_facet Arctic
Svalbard
Spitsbergen
op_source Atmosphere, Vol 12, Iss 1165, p 1165 (2021)
op_relation https://www.mdpi.com/2073-4433/12/9/1165
https://doaj.org/toc/2073-4433
doi:10.3390/atmos12091165
2073-4433
https://doaj.org/article/0e5e5cbed5264bc7887eb662fd0788b0
op_doi https://doi.org/10.3390/atmos12091165
container_title Atmosphere
container_volume 12
container_issue 9
container_start_page 1165
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