The role of the North Atlantic Oscillation in European climate projections

This study highlights the expected range of projected winter air temperature and precipitation trends over the next 30-50 years due to unpredictable fluctuations of the North Atlantic Oscillation (NAO) superimposed upon forced anthropogenic climate change. The findings are based on a 40-member initi...

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Published in:Climate Dynamics
Other Authors: Deser, Clara (author), Hurrell, James W. (author), Phillips, Adam S. (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://doi.org/10.1007/s00382-016-3502-z
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spelling ftncar:oai:drupal-site.org:articles_21147 2023-09-05T13:21:28+02:00 The role of the North Atlantic Oscillation in European climate projections Deser, Clara (author) Hurrell, James W. (author) Phillips, Adam S. (author) 2017-11-30 https://doi.org/10.1007/s00382-016-3502-z en eng Climate Dynamics--Clim Dyn--0930-7575--1432-0894 articles:21147 ark:/85065/d74q7xjm doi:10.1007/s00382-016-3502-z Copyright 2017 Springer. article Text 2017 ftncar https://doi.org/10.1007/s00382-016-3502-z 2023-08-14T18:48:58Z This study highlights the expected range of projected winter air temperature and precipitation trends over the next 30-50 years due to unpredictable fluctuations of the North Atlantic Oscillation (NAO) superimposed upon forced anthropogenic climate change. The findings are based on a 40-member initial-condition ensemble of simulations covering the period 1920-2100 conducted with the Community Earth System Model version 1 (CESM1) at 1A degrees spatial resolution. The magnitude (and in some regions, even the sign) of the projected temperature and precipitation trends over Europe, Russia and parts of the Middle East vary considerably across the ensemble depending on the evolution of the NAO in each individual member. Thus, internal variability of the NAO imparts substantial uncertainty to future changes in regional climate over the coming decades. To validate the model results, we apply a simple scaling approach that relates the margin-of-error on a trend to the statistics of the interannual variability. In this way, we can obtain the expected range of projected climate trends using the interannual statistics of the observed NAO record in combination with the model's radiatively-forced response (given by the ensemble-mean of the 40 simulations). The results of this observationally-based estimate are similar to those obtained directly from the CESM ensemble, attesting to the fidelity of the model's representation of the NAO and the utility of this approach. Finally, we note that the interannual statistics of the NAO and associated surface climate impacts are subject to uncertainty due to sampling fluctuations, even when based on a century of data. Article in Journal/Newspaper North Atlantic North Atlantic oscillation OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Climate Dynamics 49 9-10 3141 3157
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description This study highlights the expected range of projected winter air temperature and precipitation trends over the next 30-50 years due to unpredictable fluctuations of the North Atlantic Oscillation (NAO) superimposed upon forced anthropogenic climate change. The findings are based on a 40-member initial-condition ensemble of simulations covering the period 1920-2100 conducted with the Community Earth System Model version 1 (CESM1) at 1A degrees spatial resolution. The magnitude (and in some regions, even the sign) of the projected temperature and precipitation trends over Europe, Russia and parts of the Middle East vary considerably across the ensemble depending on the evolution of the NAO in each individual member. Thus, internal variability of the NAO imparts substantial uncertainty to future changes in regional climate over the coming decades. To validate the model results, we apply a simple scaling approach that relates the margin-of-error on a trend to the statistics of the interannual variability. In this way, we can obtain the expected range of projected climate trends using the interannual statistics of the observed NAO record in combination with the model's radiatively-forced response (given by the ensemble-mean of the 40 simulations). The results of this observationally-based estimate are similar to those obtained directly from the CESM ensemble, attesting to the fidelity of the model's representation of the NAO and the utility of this approach. Finally, we note that the interannual statistics of the NAO and associated surface climate impacts are subject to uncertainty due to sampling fluctuations, even when based on a century of data.
author2 Deser, Clara (author)
Hurrell, James W. (author)
Phillips, Adam S. (author)
format Article in Journal/Newspaper
title The role of the North Atlantic Oscillation in European climate projections
spellingShingle The role of the North Atlantic Oscillation in European climate projections
title_short The role of the North Atlantic Oscillation in European climate projections
title_full The role of the North Atlantic Oscillation in European climate projections
title_fullStr The role of the North Atlantic Oscillation in European climate projections
title_full_unstemmed The role of the North Atlantic Oscillation in European climate projections
title_sort role of the north atlantic oscillation in european climate projections
publishDate 2017
url https://doi.org/10.1007/s00382-016-3502-z
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Climate Dynamics--Clim Dyn--0930-7575--1432-0894
articles:21147
ark:/85065/d74q7xjm
doi:10.1007/s00382-016-3502-z
op_rights Copyright 2017 Springer.
op_doi https://doi.org/10.1007/s00382-016-3502-z
container_title Climate Dynamics
container_volume 49
container_issue 9-10
container_start_page 3141
op_container_end_page 3157
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