REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009

Arctic Oscillation (AO) reflects the dominating mode of SLP (or 1000hPa) variability in hemispheric scale and seems to bear an effect on the weather and, in longer time scales, on climate. The aim of the research was to identify the possible regime shifts in the multiannual course of AO index which...

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Main Author: Marosz, Michał
Format: Article in Journal/Newspaper
Language:English
Published: Uniwersytet Mikołaja Kopernika w Toruniu 2010
Subjects:
Online Access:https://apcz.umk.pl/BOGPGS/article/view/2331
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spelling ftapczojs:oai:apcz.umk.pl:article/2331 2023-05-15T14:48:11+02:00 REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009 Marosz, Michał 2010-12-01 application/pdf https://apcz.umk.pl/BOGPGS/article/view/2331 eng eng Uniwersytet Mikołaja Kopernika w Toruniu https://apcz.umk.pl/BOGPGS/article/view/2331/2313 https://apcz.umk.pl/BOGPGS/article/view/2331 Prawa autorskie (c) 2010 Michał Marosz https://creativecommons.org/licenses/by-nd/4.0 CC-BY-ND Bulletin of Geography. Physical Geography Series; Nr 3 (2010); 103-119 Bulletin of Geography. Physical Geography Series; No. 3 (2010); 103-119 2300-8490 2080-7686 Arctic Arctic Oscillation regime shifts info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2010 ftapczojs 2022-08-13T05:17:30Z Arctic Oscillation (AO) reflects the dominating mode of SLP (or 1000hPa) variability in hemispheric scale and seems to bear an effect on the weather and, in longer time scales, on climate. The aim of the research was to identify the possible regime shifts in the multiannual course of AO index which in turn might be utilised in the identification and quantification of the regional/local meteorological field response. The data (AO monthly and daily index values) were acquired from the NOAA Climate Prediction Centre. The AO index is constructed by projecting monthly/daily anomalies of 1000hPa heights poleward of 20°N onto the loading pattern of the AO – 1st (leading) EOF of the 1000hPa height field for the same spatial domain. The temporal scope of analysis was 1951–2009. The analysis comprised the regime shift identification techniques that track the shifts in the mean values and in the magnitude of fluctuations as well as the usage of the classical linear trend identification in the annual and seasonal scale. The regime shift recognition was followed by the compositing method that allowed the analysis of spatial anomalies in SLP field in Euro-Atlantic region that reflect the response of the regional airflow to identified circulation regimes. Article in Journal/Newspaper Arctic Akademicka Platforma Czasopism Arctic
institution Open Polar
collection Akademicka Platforma Czasopism
op_collection_id ftapczojs
language English
topic Arctic
Arctic Oscillation
regime shifts
spellingShingle Arctic
Arctic Oscillation
regime shifts
Marosz, Michał
REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009
topic_facet Arctic
Arctic Oscillation
regime shifts
description Arctic Oscillation (AO) reflects the dominating mode of SLP (or 1000hPa) variability in hemispheric scale and seems to bear an effect on the weather and, in longer time scales, on climate. The aim of the research was to identify the possible regime shifts in the multiannual course of AO index which in turn might be utilised in the identification and quantification of the regional/local meteorological field response. The data (AO monthly and daily index values) were acquired from the NOAA Climate Prediction Centre. The AO index is constructed by projecting monthly/daily anomalies of 1000hPa heights poleward of 20°N onto the loading pattern of the AO – 1st (leading) EOF of the 1000hPa height field for the same spatial domain. The temporal scope of analysis was 1951–2009. The analysis comprised the regime shift identification techniques that track the shifts in the mean values and in the magnitude of fluctuations as well as the usage of the classical linear trend identification in the annual and seasonal scale. The regime shift recognition was followed by the compositing method that allowed the analysis of spatial anomalies in SLP field in Euro-Atlantic region that reflect the response of the regional airflow to identified circulation regimes.
format Article in Journal/Newspaper
author Marosz, Michał
author_facet Marosz, Michał
author_sort Marosz, Michał
title REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009
title_short REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009
title_full REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009
title_fullStr REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009
title_full_unstemmed REGIME SHIFTS IN ARCTIC OSCILLATION (AO) VARIABILITY 1951–2009
title_sort regime shifts in arctic oscillation (ao) variability 1951–2009
publisher Uniwersytet Mikołaja Kopernika w Toruniu
publishDate 2010
url https://apcz.umk.pl/BOGPGS/article/view/2331
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Bulletin of Geography. Physical Geography Series; Nr 3 (2010); 103-119
Bulletin of Geography. Physical Geography Series; No. 3 (2010); 103-119
2300-8490
2080-7686
op_relation https://apcz.umk.pl/BOGPGS/article/view/2331/2313
https://apcz.umk.pl/BOGPGS/article/view/2331
op_rights Prawa autorskie (c) 2010 Michał Marosz
https://creativecommons.org/licenses/by-nd/4.0
op_rightsnorm CC-BY-ND
_version_ 1766319279357034496