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Title: Little influence of Arctic amplification on mid-latitude climate

Abstract

Observations and model simulations show enhanced warming in the Arctic under increasing greenhouse gases, a phenomenon known as the Arctic amplification (AA), that is likely caused by sea-ice loss. AA reduces meridional temperature gradients linked to circulation, thus mid-latitude weather and climate changes have been attributed to AA, often on the basis of regression analysis and atmospheric simulations. However, other modelling studies show only a weak link. This inconsistency may result from deficiencies in separating the effects of AA from those of natural variability or background warming. In this work, using coupled model simulations with and without AA, we show that cold-season precipitation, snowfall and circulation changes over northern mid-latitudes come mostly from background warming. AA and sea-ice loss increase precipitation and snowfall above ~60° N and reduce meridional temperature gradients above ~45° N in the lower–mid troposphere. However, minimal impact on the mean climate is seen below ~60° N, with weak reduction in zonal wind over 50°–70° N and 150–700 hPa, mainly over the North Atlantic and northern central Asia. These results suggest that the climatic impacts of AA are probably small outside the high latitudes, thus caution is needed in attributing mid-latitude changes to AA and sea-ice lossmore » on the basis of statistical analyses that cannot distinguish the impact of AA from other correlated changes.« less

Authors:
ORCiD logo [1];  [2]
  1. State Univ. of New York (SUNY), Albany, NY (United States)
  2. Chinese Academy of Sciences (CAS), Beijing (China)
Publication Date:
Research Org.:
State Univ. of New York (SUNY), Albany, NY (United States)
Sponsoring Org.:
USDOE Office of Science (SC); Chinese Academy of Sciences (CAS); National Science Foundation (NSF); US National Oceanic and Atmospheric Administration
OSTI Identifier:
1802431
Grant/Contract Number:  
SC0012602; XDA19070403; AGS-1353740; OISE-174738; NA15OAR4310086
Resource Type:
Accepted Manuscript
Journal Name:
Nature Climate Change
Additional Journal Information:
Journal Volume: 10; Journal Issue: 3; Journal ID: ISSN 1758-678X
Publisher:
Nature Publishing Group
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; environmental sciences & ecology; meteorology & atmospheric sciences; attribution; climate-change impacts

Citation Formats

Dai, Aiguo, and Song, Mirong. Little influence of Arctic amplification on mid-latitude climate. United States: N. p., 2020. Web. doi:10.1038/s41558-020-0694-3.
Dai, Aiguo, & Song, Mirong. Little influence of Arctic amplification on mid-latitude climate. United States. https://doi.org/10.1038/s41558-020-0694-3
Dai, Aiguo, and Song, Mirong. Mon . "Little influence of Arctic amplification on mid-latitude climate". United States. https://doi.org/10.1038/s41558-020-0694-3. https://www.osti.gov/servlets/purl/1802431.
@article{osti_1802431,
title = {Little influence of Arctic amplification on mid-latitude climate},
author = {Dai, Aiguo and Song, Mirong},
abstractNote = {Observations and model simulations show enhanced warming in the Arctic under increasing greenhouse gases, a phenomenon known as the Arctic amplification (AA), that is likely caused by sea-ice loss. AA reduces meridional temperature gradients linked to circulation, thus mid-latitude weather and climate changes have been attributed to AA, often on the basis of regression analysis and atmospheric simulations. However, other modelling studies show only a weak link. This inconsistency may result from deficiencies in separating the effects of AA from those of natural variability or background warming. In this work, using coupled model simulations with and without AA, we show that cold-season precipitation, snowfall and circulation changes over northern mid-latitudes come mostly from background warming. AA and sea-ice loss increase precipitation and snowfall above ~60° N and reduce meridional temperature gradients above ~45° N in the lower–mid troposphere. However, minimal impact on the mean climate is seen below ~60° N, with weak reduction in zonal wind over 50°–70° N and 150–700 hPa, mainly over the North Atlantic and northern central Asia. These results suggest that the climatic impacts of AA are probably small outside the high latitudes, thus caution is needed in attributing mid-latitude changes to AA and sea-ice loss on the basis of statistical analyses that cannot distinguish the impact of AA from other correlated changes.},
doi = {10.1038/s41558-020-0694-3},
journal = {Nature Climate Change},
number = 3,
volume = 10,
place = {United States},
year = {Mon Feb 10 00:00:00 EST 2020},
month = {Mon Feb 10 00:00:00 EST 2020}
}

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