Further investigation of NAO-winter rainfall links
The North Atlantic Oscillation (NAO) is a major atmospheric circulation feature shown to control winter precipitation amounts in Western Europe. In this short study the incorporation of absolute pressure values in the Azores and Iceland in the NAO is evaluated. In addition a comparison between the s...
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ftunorthamptoncr:oai:pure.atira.dk:publications/ba5bfb86-cf90-4f80-b19d-dbfca381581a 2023-05-15T16:47:55+02:00 Further investigation of NAO-winter rainfall links Spellman, G. 2000-03-01 https://pure.northampton.ac.uk/en/publications/ba5bfb86-cf90-4f80-b19d-dbfca381581a http://www.scopus.com/inward/record.url?eid=2-s2.0-0034024041&partnerID=MN8TOARS eng eng info:eu-repo/semantics/restrictedAccess Spellman , G 2000 , ' Further investigation of NAO-winter rainfall links ' , Journal of Applied Meteorology , vol. 25 , no. 247 , pp. 89-97 . article 2000 ftunorthamptoncr 2023-01-12T13:57:32Z The North Atlantic Oscillation (NAO) is a major atmospheric circulation feature shown to control winter precipitation amounts in Western Europe. In this short study the incorporation of absolute pressure values in the Azores and Iceland in the NAO is evaluated. In addition a comparison between the surface-based and a mid-tropospheric (500 hPa) index is made. Improvement in explanation of rainfall variability is achieved for some regions. The upper air index is found to have a stronger association with British Isles winter precipitation than the NAO itself. Article in Journal/Newspaper Iceland North Atlantic North Atlantic oscillation University of Northampton's Research Explorer |
institution |
Open Polar |
collection |
University of Northampton's Research Explorer |
op_collection_id |
ftunorthamptoncr |
language |
English |
description |
The North Atlantic Oscillation (NAO) is a major atmospheric circulation feature shown to control winter precipitation amounts in Western Europe. In this short study the incorporation of absolute pressure values in the Azores and Iceland in the NAO is evaluated. In addition a comparison between the surface-based and a mid-tropospheric (500 hPa) index is made. Improvement in explanation of rainfall variability is achieved for some regions. The upper air index is found to have a stronger association with British Isles winter precipitation than the NAO itself. |
format |
Article in Journal/Newspaper |
author |
Spellman, G. |
spellingShingle |
Spellman, G. Further investigation of NAO-winter rainfall links |
author_facet |
Spellman, G. |
author_sort |
Spellman, G. |
title |
Further investigation of NAO-winter rainfall links |
title_short |
Further investigation of NAO-winter rainfall links |
title_full |
Further investigation of NAO-winter rainfall links |
title_fullStr |
Further investigation of NAO-winter rainfall links |
title_full_unstemmed |
Further investigation of NAO-winter rainfall links |
title_sort |
further investigation of nao-winter rainfall links |
publishDate |
2000 |
url |
https://pure.northampton.ac.uk/en/publications/ba5bfb86-cf90-4f80-b19d-dbfca381581a http://www.scopus.com/inward/record.url?eid=2-s2.0-0034024041&partnerID=MN8TOARS |
genre |
Iceland North Atlantic North Atlantic oscillation |
genre_facet |
Iceland North Atlantic North Atlantic oscillation |
op_source |
Spellman , G 2000 , ' Further investigation of NAO-winter rainfall links ' , Journal of Applied Meteorology , vol. 25 , no. 247 , pp. 89-97 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1766038028252348416 |