Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover

Abstract The exceptional atmospheric conditions that have accelerated Greenland Ice Sheet mass loss in recent decades have been repeatedly recognized as a possible dynamical response to Arctic amplification. Here, we present evidence of two potentially synergistic mechanisms linking high-latitude wa...

Full description

Bibliographic Details
Published in:Nature Communications
Main Authors: Jonathon R. Preece, Thomas L. Mote, Judah Cohen, Lori J. Wachowicz, John A. Knox, Marco Tedesco, Gabriel J. Kooperman
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Q
Online Access:https://doi.org/10.1038/s41467-023-39466-6
https://doaj.org/article/f7d7385ad12a424fb568ddeb21dceda0
id ftdoajarticles:oai:doaj.org/article:f7d7385ad12a424fb568ddeb21dceda0
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:f7d7385ad12a424fb568ddeb21dceda0 2023-07-23T04:17:12+02:00 Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover Jonathon R. Preece Thomas L. Mote Judah Cohen Lori J. Wachowicz John A. Knox Marco Tedesco Gabriel J. Kooperman 2023-06-01T00:00:00Z https://doi.org/10.1038/s41467-023-39466-6 https://doaj.org/article/f7d7385ad12a424fb568ddeb21dceda0 EN eng Nature Portfolio https://doi.org/10.1038/s41467-023-39466-6 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-023-39466-6 2041-1723 https://doaj.org/article/f7d7385ad12a424fb568ddeb21dceda0 Nature Communications, Vol 14, Iss 1, Pp 1-15 (2023) Science Q article 2023 ftdoajarticles https://doi.org/10.1038/s41467-023-39466-6 2023-07-02T00:40:58Z Abstract The exceptional atmospheric conditions that have accelerated Greenland Ice Sheet mass loss in recent decades have been repeatedly recognized as a possible dynamical response to Arctic amplification. Here, we present evidence of two potentially synergistic mechanisms linking high-latitude warming to the observed increase in Greenland blocking. Consistent with a prominent hypothesis associating Arctic amplification and persistent weather extremes, we show that the summer atmospheric circulation over the North Atlantic has become wavier and link this wavier flow to more prevalent Greenland blocking. While a concomitant decline in terrestrial snow cover has likely contributed to this mechanism by further amplifying warming at high latitudes, we also show that there is a direct stationary Rossby wave response to low spring North American snow cover that enforces an anomalous anticyclone over Greenland, thus helping to anchor the ridge over Greenland in this wavier atmospheric state. Article in Journal/Newspaper Arctic Greenland Ice Sheet North Atlantic Directory of Open Access Journals: DOAJ Articles Arctic Greenland Nature Communications 14 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
Jonathon R. Preece
Thomas L. Mote
Judah Cohen
Lori J. Wachowicz
John A. Knox
Marco Tedesco
Gabriel J. Kooperman
Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover
topic_facet Science
Q
description Abstract The exceptional atmospheric conditions that have accelerated Greenland Ice Sheet mass loss in recent decades have been repeatedly recognized as a possible dynamical response to Arctic amplification. Here, we present evidence of two potentially synergistic mechanisms linking high-latitude warming to the observed increase in Greenland blocking. Consistent with a prominent hypothesis associating Arctic amplification and persistent weather extremes, we show that the summer atmospheric circulation over the North Atlantic has become wavier and link this wavier flow to more prevalent Greenland blocking. While a concomitant decline in terrestrial snow cover has likely contributed to this mechanism by further amplifying warming at high latitudes, we also show that there is a direct stationary Rossby wave response to low spring North American snow cover that enforces an anomalous anticyclone over Greenland, thus helping to anchor the ridge over Greenland in this wavier atmospheric state.
format Article in Journal/Newspaper
author Jonathon R. Preece
Thomas L. Mote
Judah Cohen
Lori J. Wachowicz
John A. Knox
Marco Tedesco
Gabriel J. Kooperman
author_facet Jonathon R. Preece
Thomas L. Mote
Judah Cohen
Lori J. Wachowicz
John A. Knox
Marco Tedesco
Gabriel J. Kooperman
author_sort Jonathon R. Preece
title Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover
title_short Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover
title_full Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover
title_fullStr Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover
title_full_unstemmed Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover
title_sort summer atmospheric circulation over greenland in response to arctic amplification and diminished spring snow cover
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41467-023-39466-6
https://doaj.org/article/f7d7385ad12a424fb568ddeb21dceda0
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Greenland
Ice Sheet
North Atlantic
genre_facet Arctic
Greenland
Ice Sheet
North Atlantic
op_source Nature Communications, Vol 14, Iss 1, Pp 1-15 (2023)
op_relation https://doi.org/10.1038/s41467-023-39466-6
https://doaj.org/toc/2041-1723
doi:10.1038/s41467-023-39466-6
2041-1723
https://doaj.org/article/f7d7385ad12a424fb568ddeb21dceda0
op_doi https://doi.org/10.1038/s41467-023-39466-6
container_title Nature Communications
container_volume 14
container_issue 1
_version_ 1772178551098834944