Relation between Northern Hemisphere winter temperatures and geomagnetic or solar activity at different QBO phases

In our previous work a dominant coupling was shown between solar and geomagnetic activity, and surface air temperature of the QBO-west and east phases, respectively. The aim of the present study is to define ‘typical’ regions of positive and negative deviations from the long-term temperature average...

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Published inJournal of atmospheric and terrestrial physics Vol. 58; no. 7; pp. 883 - 897
Main Authors Bochníček, J., Bucha, V., Hejda, P., Pýcha, J.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 1996
Subjects
Northern Hemisphere
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Summary:In our previous work a dominant coupling was shown between solar and geomagnetic activity, and surface air temperature of the QBO-west and east phases, respectively. The aim of the present study is to define ‘typical’ regions of positive and negative deviations from the long-term temperature average, to determine their magnitude and to find the conditions under which such a ‘typical’ distribution of temperature fields occurs.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
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ISSN:0021-9169
DOI:10.1016/0021-9169(95)00111-5