The occurrence of coreless winters in central Spitsbergen and their synoptic conditions

Ten warm-core winters were distinguished in the period 1975/76&#x2013;2007/08, drawing on data from the Svalbard Airport weather station in central Spitsbergen and using the conditions tm1<tmand tm&#x003E;tm+1 (t is the monthly mean temperature while m 1, m and m+1 denote subsequent winte...

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Published in:Polar Research
Main Authors: Ewa Bednorz, Krzysztof Fortuniak
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2011
Subjects:
Online Access:https://doi.org/10.3402/polar.v30i0.12218
https://doaj.org/article/f8ecfa7faca043ffb95e3df048576142
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spelling ftdoajarticles:oai:doaj.org/article:f8ecfa7faca043ffb95e3df048576142 2023-05-15T15:11:03+02:00 The occurrence of coreless winters in central Spitsbergen and their synoptic conditions Ewa Bednorz Krzysztof Fortuniak 2011-12-01T00:00:00Z https://doi.org/10.3402/polar.v30i0.12218 https://doaj.org/article/f8ecfa7faca043ffb95e3df048576142 EN eng Norwegian Polar Institute http://www.polarresearch.net/index.php/polar/article/view/12218/pdf_1 https://doaj.org/toc/0800-0395 https://doaj.org/toc/1751-8369 doi:10.3402/polar.v30i0.12218 0800-0395 1751-8369 https://doaj.org/article/f8ecfa7faca043ffb95e3df048576142 Polar Research, Vol 30, Iss 0, Pp 1-10 (2011) Spitsbergen coreless winters air temperature circulation polar climate Environmental sciences GE1-350 Oceanography GC1-1581 article 2011 ftdoajarticles https://doi.org/10.3402/polar.v30i0.12218 2022-12-30T22:49:34Z Ten warm-core winters were distinguished in the period 1975/76&#x2013;2007/08, drawing on data from the Svalbard Airport weather station in central Spitsbergen and using the conditions tm1<tmand tm&#x003E;tm+1 (t is the monthly mean temperature while m 1, m and m+1 denote subsequent winter months) and the parameter of a coreless rate, cr (the ratio of the second, a2, to the first, a1, harmonic of the annual temperature wave). Composite maps of sea-level pressure (SLP) and z 500-hPa means, and anomaly maps, were constructed separately for the mid-winter warm events and for the cold months before and after warming. Using the clustering method, different pressure patterns were recognized among the days of mid-winter warm spells. The occurrence of coreless winters in central Spitsbergen seems to be largely controlled by the position, extent and intensity of large-scale atmospheric systems, mainly the Icelandic Low. When the low spreads to the east and its centre is over the Barents Sea the inflow of air masses from the northern quadrant is observed over central Spitsbergen. This inflow of cold air of Arctic origin to the island takes place during the months preceding and following warm mid-winter events. Different circulation conditions appear when the Icelandic Low gets deeper than usual and shifts northwards, which coincides with warm spells. Sometimes a secondary cyclonic centre is located over Fram Strait and its warm sector encompasses Svalbard. Article in Journal/Newspaper Arctic Barents Sea Fram Strait Polar Research Svalbard Spitsbergen Directory of Open Access Journals: DOAJ Articles Arctic Svalbard Barents Sea Polar Research 30 1 12218
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Spitsbergen
coreless winters
air temperature
circulation
polar climate
Environmental sciences
GE1-350
Oceanography
GC1-1581
spellingShingle Spitsbergen
coreless winters
air temperature
circulation
polar climate
Environmental sciences
GE1-350
Oceanography
GC1-1581
Ewa Bednorz
Krzysztof Fortuniak
The occurrence of coreless winters in central Spitsbergen and their synoptic conditions
topic_facet Spitsbergen
coreless winters
air temperature
circulation
polar climate
Environmental sciences
GE1-350
Oceanography
GC1-1581
description Ten warm-core winters were distinguished in the period 1975/76&#x2013;2007/08, drawing on data from the Svalbard Airport weather station in central Spitsbergen and using the conditions tm1<tmand tm&#x003E;tm+1 (t is the monthly mean temperature while m 1, m and m+1 denote subsequent winter months) and the parameter of a coreless rate, cr (the ratio of the second, a2, to the first, a1, harmonic of the annual temperature wave). Composite maps of sea-level pressure (SLP) and z 500-hPa means, and anomaly maps, were constructed separately for the mid-winter warm events and for the cold months before and after warming. Using the clustering method, different pressure patterns were recognized among the days of mid-winter warm spells. The occurrence of coreless winters in central Spitsbergen seems to be largely controlled by the position, extent and intensity of large-scale atmospheric systems, mainly the Icelandic Low. When the low spreads to the east and its centre is over the Barents Sea the inflow of air masses from the northern quadrant is observed over central Spitsbergen. This inflow of cold air of Arctic origin to the island takes place during the months preceding and following warm mid-winter events. Different circulation conditions appear when the Icelandic Low gets deeper than usual and shifts northwards, which coincides with warm spells. Sometimes a secondary cyclonic centre is located over Fram Strait and its warm sector encompasses Svalbard.
format Article in Journal/Newspaper
author Ewa Bednorz
Krzysztof Fortuniak
author_facet Ewa Bednorz
Krzysztof Fortuniak
author_sort Ewa Bednorz
title The occurrence of coreless winters in central Spitsbergen and their synoptic conditions
title_short The occurrence of coreless winters in central Spitsbergen and their synoptic conditions
title_full The occurrence of coreless winters in central Spitsbergen and their synoptic conditions
title_fullStr The occurrence of coreless winters in central Spitsbergen and their synoptic conditions
title_full_unstemmed The occurrence of coreless winters in central Spitsbergen and their synoptic conditions
title_sort occurrence of coreless winters in central spitsbergen and their synoptic conditions
publisher Norwegian Polar Institute
publishDate 2011
url https://doi.org/10.3402/polar.v30i0.12218
https://doaj.org/article/f8ecfa7faca043ffb95e3df048576142
geographic Arctic
Svalbard
Barents Sea
geographic_facet Arctic
Svalbard
Barents Sea
genre Arctic
Barents Sea
Fram Strait
Polar Research
Svalbard
Spitsbergen
genre_facet Arctic
Barents Sea
Fram Strait
Polar Research
Svalbard
Spitsbergen
op_source Polar Research, Vol 30, Iss 0, Pp 1-10 (2011)
op_relation http://www.polarresearch.net/index.php/polar/article/view/12218/pdf_1
https://doaj.org/toc/0800-0395
https://doaj.org/toc/1751-8369
doi:10.3402/polar.v30i0.12218
0800-0395
1751-8369
https://doaj.org/article/f8ecfa7faca043ffb95e3df048576142
op_doi https://doi.org/10.3402/polar.v30i0.12218
container_title Polar Research
container_volume 30
container_issue 1
container_start_page 12218
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