Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain

The North Atlantic Oscillation (NAO) is the primary atmospheric-oceanic circulation/teleconnection influencing regional climate in Great Britain. As our ability to predict the NAO several months in advance increases, it is important that we improve our spatio-temporal understanding of the rainfall s...

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Bibliographic Details
Published in:Atmosphere
Main Authors: Harry West, Nevil Quinn, Michael Horswell
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
NAO
Online Access:https://doi.org/10.3390/atmos12060763
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/6/763/ 2023-08-20T04:08:13+02:00 Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain Harry West Nevil Quinn Michael Horswell agris 2021-06-13 application/pdf https://doi.org/10.3390/atmos12060763 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos12060763 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 6; Pages: 763 North Atlantic Oscillation NAO rainfall signatures spatio-temporal analysis Text 2021 ftmdpi https://doi.org/10.3390/atmos12060763 2023-08-01T01:56:41Z The North Atlantic Oscillation (NAO) is the primary atmospheric-oceanic circulation/teleconnection influencing regional climate in Great Britain. As our ability to predict the NAO several months in advance increases, it is important that we improve our spatio-temporal understanding of the rainfall signatures that the circulation produces. We undertake a high resolution spatio-temporal analysis quantifying variability in rainfall response to the NAO across Great Britain. We analyse and map monthly NAO-rainfall response variability, revealing the spatial influence of the NAO on rainfall distributions, and particularly the probability of wet and dry conditions/extremes. During the winter months, we identify spatial differences in the rainfall response to the NAO between the NW and SE areas of Britain. The NW area shows a strong and more consistent NAO-rainfall response, with greater probability of more extreme wet/dry conditions. However, greater NAO-rainfall variability during winter was found in the SE. The summer months are marked by a more spatially consistent rainfall response; however, we find that there is variability in both wet/dry magnitude and directionality. We note the implications of these spatially and temporally variable NAO-rainfall responses for regional hydrometeorological predictions and highlight the potential explanatory role of other atmospheric-oceanic circulations. Text North Atlantic North Atlantic oscillation MDPI Open Access Publishing Atmosphere 12 6 763
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic North Atlantic Oscillation
NAO
rainfall signatures
spatio-temporal analysis
spellingShingle North Atlantic Oscillation
NAO
rainfall signatures
spatio-temporal analysis
Harry West
Nevil Quinn
Michael Horswell
Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain
topic_facet North Atlantic Oscillation
NAO
rainfall signatures
spatio-temporal analysis
description The North Atlantic Oscillation (NAO) is the primary atmospheric-oceanic circulation/teleconnection influencing regional climate in Great Britain. As our ability to predict the NAO several months in advance increases, it is important that we improve our spatio-temporal understanding of the rainfall signatures that the circulation produces. We undertake a high resolution spatio-temporal analysis quantifying variability in rainfall response to the NAO across Great Britain. We analyse and map monthly NAO-rainfall response variability, revealing the spatial influence of the NAO on rainfall distributions, and particularly the probability of wet and dry conditions/extremes. During the winter months, we identify spatial differences in the rainfall response to the NAO between the NW and SE areas of Britain. The NW area shows a strong and more consistent NAO-rainfall response, with greater probability of more extreme wet/dry conditions. However, greater NAO-rainfall variability during winter was found in the SE. The summer months are marked by a more spatially consistent rainfall response; however, we find that there is variability in both wet/dry magnitude and directionality. We note the implications of these spatially and temporally variable NAO-rainfall responses for regional hydrometeorological predictions and highlight the potential explanatory role of other atmospheric-oceanic circulations.
format Text
author Harry West
Nevil Quinn
Michael Horswell
author_facet Harry West
Nevil Quinn
Michael Horswell
author_sort Harry West
title Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain
title_short Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain
title_full Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain
title_fullStr Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain
title_full_unstemmed Spatio-Temporal Variability in North Atlantic Oscillation Monthly Rainfall Signatures in Great Britain
title_sort spatio-temporal variability in north atlantic oscillation monthly rainfall signatures in great britain
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12060763
op_coverage agris
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Atmosphere; Volume 12; Issue 6; Pages: 763
op_relation Climatology
https://dx.doi.org/10.3390/atmos12060763
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12060763
container_title Atmosphere
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