Present and historical climate variability in South West England
West Cornwall is the most south westerly part of mainland United Kingdom with a strong maritime climate. This paper analyses the earliest archived instrumental meteorological records collected in West Cornwall (SW England). Observations were obtained from the Met Office archive (Camborne 1957–2010;...
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ftrepec:oai:RePEc:spr:climat:v:124:y:2014:i:1:p:221-237 2023-05-15T17:34:01+02:00 Present and historical climate variability in South West England A. Kosanic S. Harrison K. Anderson I. Kavcic http://hdl.handle.net/10.1007/s10584-014-1101-8 unknown http://hdl.handle.net/10.1007/s10584-014-1101-8 article ftrepec 2020-12-04T13:30:58Z West Cornwall is the most south westerly part of mainland United Kingdom with a strong maritime climate. This paper analyses the earliest archived instrumental meteorological records collected in West Cornwall (SW England). Observations were obtained from the Met Office archive (Camborne 1957–2010; Culdrose 1985–2011), Trengwainton Garden (1940–2010), and from the Royal Cornwall Polytechnic Society, (data for Falmouth (1880–1952) and Helston (1843–1888)). Homogeneity tests were used (Levene and Brown-Forsythe tests) to exclude any trends not related to climate variability. The data exhibit trends in annual mean and maximum temperatures over the timescales analysed, and show a general temperature increase in the 20th and 21st century. Annual and seasonal temperature change was found to vary locally with strongly positive trends in autumn, spring and summer seasons. Trends in precipitation are positive only for the 19th century and only for one station. Correlation with the North Atlantic Oscillation (NAO) index gives negative results for precipitation data. However correlation with the NAO index is positive with temperature, especially in the winter season. Return period analysis shows a decrease in intensity and frequency of extreme precipitation events in the post-1975 period (Camborne and Trengwainton Garden stations). Climate change in the 20th century and future continued warming is likely to have major implications on biodiversity in this region. Copyright Springer Science+Business Media Dordrecht 2014 Article in Journal/Newspaper North Atlantic North Atlantic oscillation RePEc (Research Papers in Economics) Cornwall ENVELOPE(-59.688,-59.688,-62.366,-62.366) |
institution |
Open Polar |
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RePEc (Research Papers in Economics) |
op_collection_id |
ftrepec |
language |
unknown |
description |
West Cornwall is the most south westerly part of mainland United Kingdom with a strong maritime climate. This paper analyses the earliest archived instrumental meteorological records collected in West Cornwall (SW England). Observations were obtained from the Met Office archive (Camborne 1957–2010; Culdrose 1985–2011), Trengwainton Garden (1940–2010), and from the Royal Cornwall Polytechnic Society, (data for Falmouth (1880–1952) and Helston (1843–1888)). Homogeneity tests were used (Levene and Brown-Forsythe tests) to exclude any trends not related to climate variability. The data exhibit trends in annual mean and maximum temperatures over the timescales analysed, and show a general temperature increase in the 20th and 21st century. Annual and seasonal temperature change was found to vary locally with strongly positive trends in autumn, spring and summer seasons. Trends in precipitation are positive only for the 19th century and only for one station. Correlation with the North Atlantic Oscillation (NAO) index gives negative results for precipitation data. However correlation with the NAO index is positive with temperature, especially in the winter season. Return period analysis shows a decrease in intensity and frequency of extreme precipitation events in the post-1975 period (Camborne and Trengwainton Garden stations). Climate change in the 20th century and future continued warming is likely to have major implications on biodiversity in this region. Copyright Springer Science+Business Media Dordrecht 2014 |
format |
Article in Journal/Newspaper |
author |
A. Kosanic S. Harrison K. Anderson I. Kavcic |
spellingShingle |
A. Kosanic S. Harrison K. Anderson I. Kavcic Present and historical climate variability in South West England |
author_facet |
A. Kosanic S. Harrison K. Anderson I. Kavcic |
author_sort |
A. Kosanic |
title |
Present and historical climate variability in South West England |
title_short |
Present and historical climate variability in South West England |
title_full |
Present and historical climate variability in South West England |
title_fullStr |
Present and historical climate variability in South West England |
title_full_unstemmed |
Present and historical climate variability in South West England |
title_sort |
present and historical climate variability in south west england |
url |
http://hdl.handle.net/10.1007/s10584-014-1101-8 |
long_lat |
ENVELOPE(-59.688,-59.688,-62.366,-62.366) |
geographic |
Cornwall |
geographic_facet |
Cornwall |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
http://hdl.handle.net/10.1007/s10584-014-1101-8 |
_version_ |
1766132707801169920 |