Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007

Variability in aspects of the hydrological cycle over the Europe-Atlantic region during the summer season is analysed for the period 1979-2007, using observational estimates, reanalyses and climate model simulations. Warming and moistening trends are evident in observations and models although decad...

Full description

Bibliographic Details
Published in:International Journal of Climatology
Main Authors: Allan, R.P., Zveryaev, I.I.
Format: Article in Journal/Newspaper
Language:unknown
Published: John Wiley & Sons 2011
Subjects:
Online Access:https://centaur.reading.ac.uk/1981/
id ftunivreading:oai:centaur.reading.ac.uk:1981
record_format openpolar
spelling ftunivreading:oai:centaur.reading.ac.uk:1981 2024-02-11T10:06:05+01:00 Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007 Allan, R.P. Zveryaev, I.I. 2011-03-15 https://centaur.reading.ac.uk/1981/ unknown John Wiley & Sons Allan, R.P. <https://centaur.reading.ac.uk/view/creators/90000870.html> orcid:0000-0003-0264-9447 and Zveryaev, I.I. (2011) Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007. International Journal of Climatology, 31 (3). pp. 337-348. ISSN 0899-8418 doi: https://doi.org/10.1002/joc.2070 <https://doi.org/10.1002/joc.2070> 551 Geology hydrology meteorology Article PeerReviewed 2011 ftunivreading https://doi.org/10.1002/joc.2070 2024-01-25T23:49:15Z Variability in aspects of the hydrological cycle over the Europe-Atlantic region during the summer season is analysed for the period 1979-2007, using observational estimates, reanalyses and climate model simulations. Warming and moistening trends are evident in observations and models although decadal changes in water vapour are not well represented by reanalyses, including the new European Centre for Medium Range Weather Forecasts (ECMWF) Interim reanalysis. Over the north Atlantic and northern Europe, observed water vapour trends are close to that expected from the temperature trends and Clausius-Clapeyron equation (7% K-1), larger than the model simulations. Precipitation over Europe is dominated by large-scale dynamics with positive phases of the North Atlantic Oscillation coinciding with drier conditions over north Europe and wetter conditions over the Mediterranean region. Evaporation trends over Europe are positive in reanalyses and models, especially for the Mediterranean region (1-3% per decade in reanalyses and climate models). Over the north Atlantic, declining precipitation combined with increased moisture contributed to an apparent rise in water vapour residence time. Maximum precipitation minus evaporation over the north Atlantic occurred during summer 1991, declining thereafter. Article in Journal/Newspaper North Atlantic North Atlantic oscillation CentAUR: Central Archive at the University of Reading International Journal of Climatology 31 3 337 348
institution Open Polar
collection CentAUR: Central Archive at the University of Reading
op_collection_id ftunivreading
language unknown
topic 551 Geology
hydrology
meteorology
spellingShingle 551 Geology
hydrology
meteorology
Allan, R.P.
Zveryaev, I.I.
Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007
topic_facet 551 Geology
hydrology
meteorology
description Variability in aspects of the hydrological cycle over the Europe-Atlantic region during the summer season is analysed for the period 1979-2007, using observational estimates, reanalyses and climate model simulations. Warming and moistening trends are evident in observations and models although decadal changes in water vapour are not well represented by reanalyses, including the new European Centre for Medium Range Weather Forecasts (ECMWF) Interim reanalysis. Over the north Atlantic and northern Europe, observed water vapour trends are close to that expected from the temperature trends and Clausius-Clapeyron equation (7% K-1), larger than the model simulations. Precipitation over Europe is dominated by large-scale dynamics with positive phases of the North Atlantic Oscillation coinciding with drier conditions over north Europe and wetter conditions over the Mediterranean region. Evaporation trends over Europe are positive in reanalyses and models, especially for the Mediterranean region (1-3% per decade in reanalyses and climate models). Over the north Atlantic, declining precipitation combined with increased moisture contributed to an apparent rise in water vapour residence time. Maximum precipitation minus evaporation over the north Atlantic occurred during summer 1991, declining thereafter.
format Article in Journal/Newspaper
author Allan, R.P.
Zveryaev, I.I.
author_facet Allan, R.P.
Zveryaev, I.I.
author_sort Allan, R.P.
title Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007
title_short Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007
title_full Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007
title_fullStr Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007
title_full_unstemmed Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007
title_sort variability in the summer season hydrological cycle over the atlantic-europe region 1979-2007
publisher John Wiley & Sons
publishDate 2011
url https://centaur.reading.ac.uk/1981/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Allan, R.P. <https://centaur.reading.ac.uk/view/creators/90000870.html> orcid:0000-0003-0264-9447 and Zveryaev, I.I. (2011) Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007. International Journal of Climatology, 31 (3). pp. 337-348. ISSN 0899-8418 doi: https://doi.org/10.1002/joc.2070 <https://doi.org/10.1002/joc.2070>
op_doi https://doi.org/10.1002/joc.2070
container_title International Journal of Climatology
container_volume 31
container_issue 3
container_start_page 337
op_container_end_page 348
_version_ 1790603507921846272