A summer climate regime over Europe modulated by the North Atlantic Oscillation

Recent summer heat waves in Europe were found to be preceded by precipitation deficits in winter. Numerical studies suggest that these phenomena are dynamically linked by land-atmosphere interactions. However, there exists as yet no complete observational evidence that connects summer climate variab...

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Published in:Hydrology and Earth System Sciences
Main Authors: G. Wang, A. J. Dolman, A. Alessandri
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/hess-15-57-2011
https://doaj.org/article/efa5d3f07e3f46ea8ee404d9e776ba5c
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author G. Wang
A. J. Dolman
A. Alessandri
author_facet G. Wang
A. J. Dolman
A. Alessandri
author_sort G. Wang
collection Directory of Open Access Journals: DOAJ Articles
container_issue 1
container_start_page 57
container_title Hydrology and Earth System Sciences
container_volume 15
description Recent summer heat waves in Europe were found to be preceded by precipitation deficits in winter. Numerical studies suggest that these phenomena are dynamically linked by land-atmosphere interactions. However, there exists as yet no complete observational evidence that connects summer climate variability to winter precipitation and the relevant circulation patterns. In this paper, we investigate the functional responses of summer mean and maximum temperature (June–August, T mean and T max ) as well as soil moisture proxied by the self-calibrating Palmer drought severity index ( scPDSI ) to preceding winter precipitation (January–March, P JFM ) for the period 1901–2005. All the analyzed summer fields show distinctive responses to P JFM over the Mediterranean. We estimate that 10 ~ 15% of the interannual variability of T max and T mean over the Mediterranean is statistically forced by P JFM . For the scPDSI this amounts to 10 ~ 25%. Further analysis shows that these responses are highly correlated to the North Atlantic Oscillation (NAO) regime over the Mediterranean. We suggest that NAO modulates European summer temperature by controlling winter precipitation that initializes the moisture states that subsequently interact with temperature. This picture of relations between European summer climate and NAO as well as winter precipitation suggests potential for improved seasonal prediction of summer climate for particular extreme events.
format Article in Journal/Newspaper
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
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spelling ftdoajarticles:oai:doaj.org/article:efa5d3f07e3f46ea8ee404d9e776ba5c 2025-01-16T23:36:48+00:00 A summer climate regime over Europe modulated by the North Atlantic Oscillation G. Wang A. J. Dolman A. Alessandri 2011-01-01T00:00:00Z https://doi.org/10.5194/hess-15-57-2011 https://doaj.org/article/efa5d3f07e3f46ea8ee404d9e776ba5c EN eng Copernicus Publications http://www.hydrol-earth-syst-sci.net/15/57/2011/hess-15-57-2011.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 doi:10.5194/hess-15-57-2011 1027-5606 1607-7938 https://doaj.org/article/efa5d3f07e3f46ea8ee404d9e776ba5c Hydrology and Earth System Sciences, Vol 15, Iss 1, Pp 57-64 (2011) Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2011 ftdoajarticles https://doi.org/10.5194/hess-15-57-2011 2022-12-31T04:56:17Z Recent summer heat waves in Europe were found to be preceded by precipitation deficits in winter. Numerical studies suggest that these phenomena are dynamically linked by land-atmosphere interactions. However, there exists as yet no complete observational evidence that connects summer climate variability to winter precipitation and the relevant circulation patterns. In this paper, we investigate the functional responses of summer mean and maximum temperature (June–August, T mean and T max ) as well as soil moisture proxied by the self-calibrating Palmer drought severity index ( scPDSI ) to preceding winter precipitation (January–March, P JFM ) for the period 1901–2005. All the analyzed summer fields show distinctive responses to P JFM over the Mediterranean. We estimate that 10 ~ 15% of the interannual variability of T max and T mean over the Mediterranean is statistically forced by P JFM . For the scPDSI this amounts to 10 ~ 25%. Further analysis shows that these responses are highly correlated to the North Atlantic Oscillation (NAO) regime over the Mediterranean. We suggest that NAO modulates European summer temperature by controlling winter precipitation that initializes the moisture states that subsequently interact with temperature. This picture of relations between European summer climate and NAO as well as winter precipitation suggests potential for improved seasonal prediction of summer climate for particular extreme events. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Hydrology and Earth System Sciences 15 1 57 64
spellingShingle Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
G. Wang
A. J. Dolman
A. Alessandri
A summer climate regime over Europe modulated by the North Atlantic Oscillation
title A summer climate regime over Europe modulated by the North Atlantic Oscillation
title_full A summer climate regime over Europe modulated by the North Atlantic Oscillation
title_fullStr A summer climate regime over Europe modulated by the North Atlantic Oscillation
title_full_unstemmed A summer climate regime over Europe modulated by the North Atlantic Oscillation
title_short A summer climate regime over Europe modulated by the North Atlantic Oscillation
title_sort summer climate regime over europe modulated by the north atlantic oscillation
topic Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
topic_facet Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
url https://doi.org/10.5194/hess-15-57-2011
https://doaj.org/article/efa5d3f07e3f46ea8ee404d9e776ba5c