Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures

Abstract This study examines intercontinental linkages between late spring and early summer Eurasian snow cover extent (SCE ss ) anomalies and the following winter temperature anomalies over Canada for the 1972–2006 period. The structure of the second interannual mode of Canadian winter temperatures...

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Published in:International Journal of Climatology
Main Authors: Shabbar, Amir, Zhao, Hongxu
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2011
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.2426
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.2426
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spelling crwiley:10.1002/joc.2426 2024-06-02T08:11:16+00:00 Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures Shabbar, Amir Zhao, Hongxu 2011 http://dx.doi.org/10.1002/joc.2426 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.2426 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.2426 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 32, issue 14, page 2124-2133 ISSN 0899-8418 1097-0088 journal-article 2011 crwiley https://doi.org/10.1002/joc.2426 2024-05-03T11:59:12Z Abstract This study examines intercontinental linkages between late spring and early summer Eurasian snow cover extent (SCE ss ) anomalies and the following winter temperature anomalies over Canada for the 1972–2006 period. The structure of the second interannual mode of Canadian winter temperatures variability captures the SCE ss related modulation. The North Atlantic winter atmospheric circulation changes associated with the SCE ss , resembling the negative phase of the North Atlantic Oscillation (NAO), suggest a possible pathway for the SCE ss influences on the Canadian winter temperatures. Regression and composite analyses show that the SCE ss relate robustly to the Canadian winter climate. Larger‐than‐normal SCE ss is associated with below normal winter temperatures in south‐central Canada and above normal temperatures over northeastern Canada. Predictive skill of Canadian winter temperatures based on a cross‐validated regression model shows that the SCE ss offers the predictive potential over regions of Canada where El Niño‐Southern Oscillation (ENSO) related skill is weak or nonexistent. Analysis of winter extreme minimum temperatures, by a non‐stationary generalized extreme value model, with the SCE ss as a covariate, exhibits statistically significant changes over Canada resembling a pattern similar to that of winter mean temperatures. Wavelet analysis shows significant coherence between the SCE ss and the second mode of winter temperature variability in the 8–12‐year band. Copyright © 2011 Crown in the right of Canada. Published by John Wiley & Sons, Ltd Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library Canada International Journal of Climatology 32 14 2124 2133
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract This study examines intercontinental linkages between late spring and early summer Eurasian snow cover extent (SCE ss ) anomalies and the following winter temperature anomalies over Canada for the 1972–2006 period. The structure of the second interannual mode of Canadian winter temperatures variability captures the SCE ss related modulation. The North Atlantic winter atmospheric circulation changes associated with the SCE ss , resembling the negative phase of the North Atlantic Oscillation (NAO), suggest a possible pathway for the SCE ss influences on the Canadian winter temperatures. Regression and composite analyses show that the SCE ss relate robustly to the Canadian winter climate. Larger‐than‐normal SCE ss is associated with below normal winter temperatures in south‐central Canada and above normal temperatures over northeastern Canada. Predictive skill of Canadian winter temperatures based on a cross‐validated regression model shows that the SCE ss offers the predictive potential over regions of Canada where El Niño‐Southern Oscillation (ENSO) related skill is weak or nonexistent. Analysis of winter extreme minimum temperatures, by a non‐stationary generalized extreme value model, with the SCE ss as a covariate, exhibits statistically significant changes over Canada resembling a pattern similar to that of winter mean temperatures. Wavelet analysis shows significant coherence between the SCE ss and the second mode of winter temperature variability in the 8–12‐year band. Copyright © 2011 Crown in the right of Canada. Published by John Wiley & Sons, Ltd
format Article in Journal/Newspaper
author Shabbar, Amir
Zhao, Hongxu
spellingShingle Shabbar, Amir
Zhao, Hongxu
Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures
author_facet Shabbar, Amir
Zhao, Hongxu
author_sort Shabbar, Amir
title Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures
title_short Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures
title_full Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures
title_fullStr Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures
title_full_unstemmed Contribution of late spring Eurasian snow cover extent to Canadian winter temperatures
title_sort contribution of late spring eurasian snow cover extent to canadian winter temperatures
publisher Wiley
publishDate 2011
url http://dx.doi.org/10.1002/joc.2426
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.2426
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.2426
geographic Canada
geographic_facet Canada
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source International Journal of Climatology
volume 32, issue 14, page 2124-2133
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.2426
container_title International Journal of Climatology
container_volume 32
container_issue 14
container_start_page 2124
op_container_end_page 2133
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