Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015)

This paper discusses the cloud cover and its relation to atmospheric circulation over Spitsbergen during 1983-2015. It focuses on monthly and seasonal cloud covers and on the frequency of days with specific cloud cover (cloudless, clear, cloudy and completely overcast sky) and their relation to vari...

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Published in:Geographia Polonica
Main Authors: Łupikasza, Ewa, Lipiński, Oskar
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://hdl.handle.net/20.500.12128/14329
https://doi.org/10.7163/GPol.0076
id ftunivsilesia:oai:rebus.us.edu.pl:20.500.12128/14329
record_format openpolar
spelling ftunivsilesia:oai:rebus.us.edu.pl:20.500.12128/14329 2023-05-15T15:04:03+02:00 Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015) Łupikasza, Ewa Lipiński, Oskar 2017 https://hdl.handle.net/20.500.12128/14329 https://doi.org/10.7163/GPol.0076 en eng "Geographia Polonica" (2017), Vol. 90, iss. 1, s. 21-38 2300-7362 http://hdl.handle.net/20.500.12128/14329 doi:10.7163/GPol.0076 Uznanie autorstwa-Na tych samych warunkach 3.0 Polska http://creativecommons.org/licenses/by-sa/3.0/pl/ CC-BY-SA cloud cover atmospheric circulation Spitsbergen the Arctic info:eu-repo/semantics/article 2017 ftunivsilesia https://doi.org/20.500.12128/14329 https://doi.org/10.7163/GPol.0076 2022-12-31T20:13:41Z This paper discusses the cloud cover and its relation to atmospheric circulation over Spitsbergen during 1983-2015. It focuses on monthly and seasonal cloud covers and on the frequency of days with specific cloud cover (cloudless, clear, cloudy and completely overcast sky) and their relation to various circulation types. In the research period the cloud cover characteristics were differentiated over the island on both monthly and seasonal scales, and they strongly depended on the direction of air advection. The highest mean daily cloud cover was reported for circulation types with air advection from the south (S+SWc and S+SWa). The greatest variation in the cloud cover distribution was observed during the polar night (at Svalbard Lufthavn and Ny-Ålesund) or in the autumn (Hornsund). The long-term variability in the cloud cover significantly depends on the frequency of N+NEa type (negative correlation) and on S+SWc and W+NWc and Cc+Bc types (positive correlation), particularly in spring. Article in Journal/Newspaper Arctic Hornsund Ny Ålesund Ny-Ålesund polar night Svalbard Spitsbergen The Repository of the University of Silesia (RE-BUŚ) Arctic Svalbard Ny-Ålesund Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Geographia Polonica 90 1 21 38
institution Open Polar
collection The Repository of the University of Silesia (RE-BUŚ)
op_collection_id ftunivsilesia
language English
topic cloud cover
atmospheric circulation
Spitsbergen
the Arctic
spellingShingle cloud cover
atmospheric circulation
Spitsbergen
the Arctic
Łupikasza, Ewa
Lipiński, Oskar
Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015)
topic_facet cloud cover
atmospheric circulation
Spitsbergen
the Arctic
description This paper discusses the cloud cover and its relation to atmospheric circulation over Spitsbergen during 1983-2015. It focuses on monthly and seasonal cloud covers and on the frequency of days with specific cloud cover (cloudless, clear, cloudy and completely overcast sky) and their relation to various circulation types. In the research period the cloud cover characteristics were differentiated over the island on both monthly and seasonal scales, and they strongly depended on the direction of air advection. The highest mean daily cloud cover was reported for circulation types with air advection from the south (S+SWc and S+SWa). The greatest variation in the cloud cover distribution was observed during the polar night (at Svalbard Lufthavn and Ny-Ålesund) or in the autumn (Hornsund). The long-term variability in the cloud cover significantly depends on the frequency of N+NEa type (negative correlation) and on S+SWc and W+NWc and Cc+Bc types (positive correlation), particularly in spring.
format Article in Journal/Newspaper
author Łupikasza, Ewa
Lipiński, Oskar
author_facet Łupikasza, Ewa
Lipiński, Oskar
author_sort Łupikasza, Ewa
title Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015)
title_short Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015)
title_full Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015)
title_fullStr Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015)
title_full_unstemmed Cloud cover over Spitsbergen and its relation to atmospheric circulation (1983-2015)
title_sort cloud cover over spitsbergen and its relation to atmospheric circulation (1983-2015)
publishDate 2017
url https://hdl.handle.net/20.500.12128/14329
https://doi.org/10.7163/GPol.0076
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
geographic Arctic
Svalbard
Ny-Ålesund
Hornsund
geographic_facet Arctic
Svalbard
Ny-Ålesund
Hornsund
genre Arctic
Hornsund
Ny Ålesund
Ny-Ålesund
polar night
Svalbard
Spitsbergen
genre_facet Arctic
Hornsund
Ny Ålesund
Ny-Ålesund
polar night
Svalbard
Spitsbergen
op_relation "Geographia Polonica" (2017), Vol. 90, iss. 1, s. 21-38
2300-7362
http://hdl.handle.net/20.500.12128/14329
doi:10.7163/GPol.0076
op_rights Uznanie autorstwa-Na tych samych warunkach 3.0 Polska
http://creativecommons.org/licenses/by-sa/3.0/pl/
op_rightsnorm CC-BY-SA
op_doi https://doi.org/20.500.12128/14329
https://doi.org/10.7163/GPol.0076
container_title Geographia Polonica
container_volume 90
container_issue 1
container_start_page 21
op_container_end_page 38
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