Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects

Arguably, the most conspicuous evidence for anthropogenic climate change lies in the Arctic Ocean. For example, the summer-time Arctic sea ice extent has declined over the last 40 years and the Arctic Ocean freshwater storage has increased over the last 30 years. Coupled climate models project that...

Full description

Bibliographic Details
Published in:Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Haine, Thomas W. N., Siddiqui, Ali H., Jiang, Wenrui
Other Authors: National Aeronautics and Space Administration
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 2023
Subjects:
Online Access:http://dx.doi.org/10.1098/rsta.2022.0185
https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2022.0185
https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2022.0185
id crroyalsociety:10.1098/rsta.2022.0185
record_format openpolar
spelling crroyalsociety:10.1098/rsta.2022.0185 2024-06-02T08:00:23+00:00 Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects Haine, Thomas W. N. Siddiqui, Ali H. Jiang, Wenrui National Aeronautics and Space Administration 2023 http://dx.doi.org/10.1098/rsta.2022.0185 https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2022.0185 https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2022.0185 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences volume 381, issue 2262 ISSN 1364-503X 1471-2962 journal-article 2023 crroyalsociety https://doi.org/10.1098/rsta.2022.0185 2024-05-07T14:16:39Z Arguably, the most conspicuous evidence for anthropogenic climate change lies in the Arctic Ocean. For example, the summer-time Arctic sea ice extent has declined over the last 40 years and the Arctic Ocean freshwater storage has increased over the last 30 years. Coupled climate models project that this extra freshwater will pass Greenland to enter the sub-polar North Atlantic Ocean (SPNA) in the coming decades. Coupled climate models also project that the Atlantic Meridional Overturning Circulation (AMOC) will weaken in the twenty-first century, associated with SPNA buoyancy increases. Yet, it remains unclear when the Arctic anthropogenic freshening signal will be detected in the SPNA, or what form the signal will take. Therefore, this article reviews and synthesizes the state of knowledge on Arctic Ocean and SPNA salinity variations and their causes. This article focuses on the export processes in data-constrained ocean circulation model hindcasts. One challenge is to quantify and understand the relative importance of different competing processes. This article also discusses the prospects to detect the emergence of Arctic anthropogenic freshening and the likely impacts on the AMOC. For this issue, the challenge is to distinguish anthropogenic signals from natural variability. This article is part of a discussion meeting issue ‘Atlantic overturning: new observations and challenges’. Article in Journal/Newspaper Arctic Arctic Ocean Climate change Greenland North Atlantic Sea ice The Royal Society Arctic Arctic Ocean Greenland Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 381 2262
institution Open Polar
collection The Royal Society
op_collection_id crroyalsociety
language English
description Arguably, the most conspicuous evidence for anthropogenic climate change lies in the Arctic Ocean. For example, the summer-time Arctic sea ice extent has declined over the last 40 years and the Arctic Ocean freshwater storage has increased over the last 30 years. Coupled climate models project that this extra freshwater will pass Greenland to enter the sub-polar North Atlantic Ocean (SPNA) in the coming decades. Coupled climate models also project that the Atlantic Meridional Overturning Circulation (AMOC) will weaken in the twenty-first century, associated with SPNA buoyancy increases. Yet, it remains unclear when the Arctic anthropogenic freshening signal will be detected in the SPNA, or what form the signal will take. Therefore, this article reviews and synthesizes the state of knowledge on Arctic Ocean and SPNA salinity variations and their causes. This article focuses on the export processes in data-constrained ocean circulation model hindcasts. One challenge is to quantify and understand the relative importance of different competing processes. This article also discusses the prospects to detect the emergence of Arctic anthropogenic freshening and the likely impacts on the AMOC. For this issue, the challenge is to distinguish anthropogenic signals from natural variability. This article is part of a discussion meeting issue ‘Atlantic overturning: new observations and challenges’.
author2 National Aeronautics and Space Administration
format Article in Journal/Newspaper
author Haine, Thomas W. N.
Siddiqui, Ali H.
Jiang, Wenrui
spellingShingle Haine, Thomas W. N.
Siddiqui, Ali H.
Jiang, Wenrui
Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects
author_facet Haine, Thomas W. N.
Siddiqui, Ali H.
Jiang, Wenrui
author_sort Haine, Thomas W. N.
title Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects
title_short Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects
title_full Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects
title_fullStr Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects
title_full_unstemmed Arctic freshwater impact on the Atlantic Meridional Overturning Circulation: status and prospects
title_sort arctic freshwater impact on the atlantic meridional overturning circulation: status and prospects
publisher The Royal Society
publishDate 2023
url http://dx.doi.org/10.1098/rsta.2022.0185
https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2022.0185
https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2022.0185
geographic Arctic
Arctic Ocean
Greenland
geographic_facet Arctic
Arctic Ocean
Greenland
genre Arctic
Arctic Ocean
Climate change
Greenland
North Atlantic
Sea ice
genre_facet Arctic
Arctic Ocean
Climate change
Greenland
North Atlantic
Sea ice
op_source Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
volume 381, issue 2262
ISSN 1364-503X 1471-2962
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rsta.2022.0185
container_title Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
container_volume 381
container_issue 2262
_version_ 1800744387721822208