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Historical Trends and Variability in Heat Waves in the United Kingdom
Increases in numbers and lengths of heat waves have previously been identified in global temperature records, including locations within Europe. However, studies of changes in UK heat wave characteristics are limited. Historic daily maximum temperatures from 29 weather stations with records exceedin...
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Published in: | Atmosphere 2017-09, Vol.8 (10), p.191 |
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description | Increases in numbers and lengths of heat waves have previously been identified in global temperature records, including locations within Europe. However, studies of changes in UK heat wave characteristics are limited. Historic daily maximum temperatures from 29 weather stations with records exceeding 85 years in length across the country were examined. Heat waves were defined as periods with unusually high temperatures for each station, even if the temperatures would not be considered warm in an absolute sense. Positive trends in numbers and lengths of heat waves were identified at some stations. However, for some stations in the south east of England, lengths of very long heat waves (over 10 days) had declined since the 1970s, whereas the lengths of shorter heat waves had increased slightly. Considerable multidecadal variability in heat wave numbers and lengths was apparent at all stations. Logistic regression, using a subset of eight stations with records beginning in the nineteenth century, suggested an association between the Atlantic Multidecadal Oscillation and the variability in heat wave numbers and lengths, with the summertime North Atlantic Oscillation playing a smaller role. The results were robust against different temperature thresholds. |
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However, studies of changes in UK heat wave characteristics are limited. Historic daily maximum temperatures from 29 weather stations with records exceeding 85 years in length across the country were examined. Heat waves were defined as periods with unusually high temperatures for each station, even if the temperatures would not be considered warm in an absolute sense. Positive trends in numbers and lengths of heat waves were identified at some stations. However, for some stations in the south east of England, lengths of very long heat waves (over 10 days) had declined since the 1970s, whereas the lengths of shorter heat waves had increased slightly. Considerable multidecadal variability in heat wave numbers and lengths was apparent at all stations. Logistic regression, using a subset of eight stations with records beginning in the nineteenth century, suggested an association between the Atlantic Multidecadal Oscillation and the variability in heat wave numbers and lengths, with the summertime North Atlantic Oscillation playing a smaller role. 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However, studies of changes in UK heat wave characteristics are limited. Historic daily maximum temperatures from 29 weather stations with records exceeding 85 years in length across the country were examined. Heat waves were defined as periods with unusually high temperatures for each station, even if the temperatures would not be considered warm in an absolute sense. Positive trends in numbers and lengths of heat waves were identified at some stations. However, for some stations in the south east of England, lengths of very long heat waves (over 10 days) had declined since the 1970s, whereas the lengths of shorter heat waves had increased slightly. Considerable multidecadal variability in heat wave numbers and lengths was apparent at all stations. Logistic regression, using a subset of eight stations with records beginning in the nineteenth century, suggested an association between the Atlantic Multidecadal Oscillation and the variability in heat wave numbers and lengths, with the summertime North Atlantic Oscillation playing a smaller role. The results were robust against different temperature thresholds.</description><subject>AMO</subject><subject>Atmospheric forcing</subject><subject>climate variability</subject><subject>Global temperatures</subject><subject>Heat</subject><subject>Heat waves</subject><subject>Heatwaves</subject><subject>High temperature</subject><subject>Historic temperatures</subject><subject>Identification</subject><subject>logistic regression</subject><subject>Maximum temperatures</subject><subject>NAO</subject><subject>North Atlantic Oscillation</subject><subject>Ocean-atmosphere system</subject><subject>Records</subject><subject>Temperature</subject><subject>Temperature effects</subject><subject>Trends</subject><subject>Variability</subject><subject>Wavelengths</subject><subject>Weather stations</subject><issn>2073-4433</issn><issn>2073-4433</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNpNkEtLAzEUhYMoWGp3_oCAW6t5zWSylFJtseCm1WW4k2RqynRSk1Tov3dqRXo398HhO5eD0C0lD5wr8gh5G1JFCaGKXqABI5KPheD88my-RqOUNqQvoTjjYoCmM59yiN5Ai5fRdTZh6Cx-h-ih9q3PB-w7PHOQ8Qd8u3Tc8qfDq85nZ_Gr79Y2bG_QVQNtcqO_PkSr5-lyMhsv3l7mk6fF2PBS5jGjjRGUyKIqwEhoaGWNUQoIN3VJSSW5KKW1tHGyYEbWyjleKFVaUcmCK8eHaH7i2gAbvYt-C_GgA3j9ewhxrSFmb1qnKbjaAmG1LKQwBGoHjeCqkcRyxhjpWXcn1i6Gr71LWW_CPnb9-5qqsigUYRXtVfcnlYkhpeiaf1dK9DF3fZ47_wHpYHRi</recordid><startdate>20170930</startdate><enddate>20170930</enddate><creator>Sanderson, Michael</creator><creator>Economou, Theo</creator><creator>Salmon, Kate</creator><creator>Jones, Sarah</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>SOI</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0001-8697-1518</orcidid><orcidid>https://orcid.org/0000-0001-8123-8237</orcidid></search><sort><creationdate>20170930</creationdate><title>Historical Trends and Variability in Heat Waves in the United Kingdom</title><author>Sanderson, Michael ; 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subjects | AMO Atmospheric forcing climate variability Global temperatures Heat Heat waves Heatwaves High temperature Historic temperatures Identification logistic regression Maximum temperatures NAO North Atlantic Oscillation Ocean-atmosphere system Records Temperature Temperature effects Trends Variability Wavelengths Weather stations |
title | Historical Trends and Variability in Heat Waves in the United Kingdom |
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