Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region

Arctic Amplification of climate warming is caused by various feedback processes in the atmosphere-ocean-ice system and yields the strongest temperature increase during winter in the Arctic North Atlantic region. In our study, we attempt to quantify the advective contribution to the observed atmosphe...

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Main Authors: Sandro Dahlke, Marion Maturilli
Format: Article
Language:English
Published: Wiley 2017-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2017/4928620
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author Sandro Dahlke
Marion Maturilli
author_facet Sandro Dahlke
Marion Maturilli
author_sort Sandro Dahlke
collection DOAJ
description Arctic Amplification of climate warming is caused by various feedback processes in the atmosphere-ocean-ice system and yields the strongest temperature increase during winter in the Arctic North Atlantic region. In our study, we attempt to quantify the advective contribution to the observed atmospheric warming in the Svalbard area. Based on radiosonde measurements from Ny-Ålesund, a strong dependence of the tropospheric temperature on the synoptic flow direction is revealed. Using FLEXTRA backward trajectories, an increase of advection from the lower latitude Atlantic region towards Ny-Ålesund is found that is attributed to a change in atmospheric circulation patterns. We find that about one-quarter (0.45 K per decade) of the observed atmospheric winter near surface warming trend in the North Atlantic region of the Arctic (2 K per decade) is due to increased advection of warm and moist air from the lower latitude Atlantic region, affecting the entire troposphere.
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spelling doaj-art-dc5fde96d8b84daaa9c2aa17bfff11fa2025-08-20T02:21:37ZengWileyAdvances in Meteorology1687-93091687-93172017-01-01201710.1155/2017/49286204928620Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic RegionSandro Dahlke0Marion Maturilli1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, GermanyAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, GermanyArctic Amplification of climate warming is caused by various feedback processes in the atmosphere-ocean-ice system and yields the strongest temperature increase during winter in the Arctic North Atlantic region. In our study, we attempt to quantify the advective contribution to the observed atmospheric warming in the Svalbard area. Based on radiosonde measurements from Ny-Ålesund, a strong dependence of the tropospheric temperature on the synoptic flow direction is revealed. Using FLEXTRA backward trajectories, an increase of advection from the lower latitude Atlantic region towards Ny-Ålesund is found that is attributed to a change in atmospheric circulation patterns. We find that about one-quarter (0.45 K per decade) of the observed atmospheric winter near surface warming trend in the North Atlantic region of the Arctic (2 K per decade) is due to increased advection of warm and moist air from the lower latitude Atlantic region, affecting the entire troposphere.http://dx.doi.org/10.1155/2017/4928620
spellingShingle Sandro Dahlke
Marion Maturilli
Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region
Advances in Meteorology
title Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region
title_full Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region
title_fullStr Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region
title_full_unstemmed Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region
title_short Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region
title_sort contribution of atmospheric advection to the amplified winter warming in the arctic north atlantic region
url http://dx.doi.org/10.1155/2017/4928620
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AT marionmaturilli contributionofatmosphericadvectiontotheamplifiedwinterwarminginthearcticnorthatlanticregion