European precipitation connections with large-scale mean sea-level pressure (MSLP) fields

To advance understanding of hydroclimatological processes, this paper links spatiotemporal variability in gridded European precipitation and large-scale mean sea-level pressure (MSLP) time series (1957–2002) using monthly concurrent correlation. Strong negative (positive) correlation near Iceland an...

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Published in:Hydrological Sciences Journal
Main Authors: Lavers, David, Prudhomme, Christel, Hannah, David M.
Format: Article in Journal/Newspaper
Language:unknown
Published: Taylor & Francis 2013
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/13448/
https://doi.org/10.1080/02626667.2012.754545
id ftnerc:oai:nora.nerc.ac.uk:13448
record_format openpolar
spelling ftnerc:oai:nora.nerc.ac.uk:13448 2023-05-15T16:49:49+02:00 European precipitation connections with large-scale mean sea-level pressure (MSLP) fields Lavers, David Prudhomme, Christel Hannah, David M. 2013 http://nora.nerc.ac.uk/id/eprint/13448/ https://doi.org/10.1080/02626667.2012.754545 unknown Taylor & Francis Lavers, David; Prudhomme, Christel; Hannah, David M. 2013 European precipitation connections with large-scale mean sea-level pressure (MSLP) fields. Hydrological Sciences Journal, 58 (2). 310-327. https://doi.org/10.1080/02626667.2012.754545 <https://doi.org/10.1080/02626667.2012.754545> Meteorology and Climatology Hydrology Publication - Article PeerReviewed 2013 ftnerc https://doi.org/10.1080/02626667.2012.754545 2023-02-04T19:28:39Z To advance understanding of hydroclimatological processes, this paper links spatiotemporal variability in gridded European precipitation and large-scale mean sea-level pressure (MSLP) time series (1957–2002) using monthly concurrent correlation. Strong negative (positive) correlation near Iceland and (the Azores) is apparent for precipitation in northwest Europe, confirming a positive North Atlantic Oscillation (NAO) association. An opposing pattern is found for southwest Europe, and the Mediterranean in winter. In the lee of mountains, MSLP correlation is lower reflecting reduced influence of westerlies on precipitation generation. Importantly, European precipitation is shown to be controlled by physically interpretable climate patterns that change in extent and position from month to month. In spring, MSLP–precipitation correlation patterns move and shrink, reaching a minimum in summer, before expanding in the autumn, and forming an NAO-like dipole in winter. These space–time shifts in correlation regions explain why fixed-point NAO indices have limited ability to resolve precipitation for some European locations and seasons. Article in Journal/Newspaper Iceland North Atlantic North Atlantic oscillation Natural Environment Research Council: NERC Open Research Archive Hydrological Sciences Journal 58 2 310 327
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
topic Meteorology and Climatology
Hydrology
spellingShingle Meteorology and Climatology
Hydrology
Lavers, David
Prudhomme, Christel
Hannah, David M.
European precipitation connections with large-scale mean sea-level pressure (MSLP) fields
topic_facet Meteorology and Climatology
Hydrology
description To advance understanding of hydroclimatological processes, this paper links spatiotemporal variability in gridded European precipitation and large-scale mean sea-level pressure (MSLP) time series (1957–2002) using monthly concurrent correlation. Strong negative (positive) correlation near Iceland and (the Azores) is apparent for precipitation in northwest Europe, confirming a positive North Atlantic Oscillation (NAO) association. An opposing pattern is found for southwest Europe, and the Mediterranean in winter. In the lee of mountains, MSLP correlation is lower reflecting reduced influence of westerlies on precipitation generation. Importantly, European precipitation is shown to be controlled by physically interpretable climate patterns that change in extent and position from month to month. In spring, MSLP–precipitation correlation patterns move and shrink, reaching a minimum in summer, before expanding in the autumn, and forming an NAO-like dipole in winter. These space–time shifts in correlation regions explain why fixed-point NAO indices have limited ability to resolve precipitation for some European locations and seasons.
format Article in Journal/Newspaper
author Lavers, David
Prudhomme, Christel
Hannah, David M.
author_facet Lavers, David
Prudhomme, Christel
Hannah, David M.
author_sort Lavers, David
title European precipitation connections with large-scale mean sea-level pressure (MSLP) fields
title_short European precipitation connections with large-scale mean sea-level pressure (MSLP) fields
title_full European precipitation connections with large-scale mean sea-level pressure (MSLP) fields
title_fullStr European precipitation connections with large-scale mean sea-level pressure (MSLP) fields
title_full_unstemmed European precipitation connections with large-scale mean sea-level pressure (MSLP) fields
title_sort european precipitation connections with large-scale mean sea-level pressure (mslp) fields
publisher Taylor & Francis
publishDate 2013
url http://nora.nerc.ac.uk/id/eprint/13448/
https://doi.org/10.1080/02626667.2012.754545
genre Iceland
North Atlantic
North Atlantic oscillation
genre_facet Iceland
North Atlantic
North Atlantic oscillation
op_relation Lavers, David; Prudhomme, Christel; Hannah, David M. 2013 European precipitation connections with large-scale mean sea-level pressure (MSLP) fields. Hydrological Sciences Journal, 58 (2). 310-327. https://doi.org/10.1080/02626667.2012.754545 <https://doi.org/10.1080/02626667.2012.754545>
op_doi https://doi.org/10.1080/02626667.2012.754545
container_title Hydrological Sciences Journal
container_volume 58
container_issue 2
container_start_page 310
op_container_end_page 327
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