Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century
Abstract The enhanced warming of the Arctic, relative to other parts of the Earth, a phenomenon known as Arctic amplification, is one of the most striking features of climate change, and has important climatic impacts for the entire Northern Hemisphere. Several mechanisms are believed to be responsi...
Guardado en:
Autores principales: | , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2021
|
Materias: | |
Acceso en línea: | https://doaj.org/article/61048e2ffade48e78ba570dc1492ca84 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:61048e2ffade48e78ba570dc1492ca84 |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:61048e2ffade48e78ba570dc1492ca842021-12-02T19:16:12ZQuantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century10.1038/s41612-021-00204-82397-3722https://doaj.org/article/61048e2ffade48e78ba570dc1492ca842021-10-01T00:00:00Zhttps://doi.org/10.1038/s41612-021-00204-8https://doaj.org/toc/2397-3722Abstract The enhanced warming of the Arctic, relative to other parts of the Earth, a phenomenon known as Arctic amplification, is one of the most striking features of climate change, and has important climatic impacts for the entire Northern Hemisphere. Several mechanisms are believed to be responsible for Arctic amplification; however, a quantitative understanding of their relative importance is still missing. Here, using ensembles of model integrations, we quantify the contribution of ocean coupling, both its thermodynamic and dynamic components, to Arctic amplification over the 20th and 21st centuries. We show that ocean coupling accounts for ~80% of the amplification by 2100. In particular, we show that thermodynamic coupling is responsible for future amplification and sea-ice loss as it overcomes the effect of dynamic coupling which reduces the amplification and sea-ice loss by ~35%. Our results demonstrate the utility of targeted numerical experiments to quantify the role of specific mechanisms in Arctic amplification, for better constraining climate projections.Rei ChemkeLorenzo M. PolvaniJennifer E. KayClara OrbeNature PortfolioarticleEnvironmental sciencesGE1-350Meteorology. ClimatologyQC851-999ENnpj Climate and Atmospheric Science, Vol 4, Iss 1, Pp 1-9 (2021) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Rei Chemke Lorenzo M. Polvani Jennifer E. Kay Clara Orbe Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century |
description |
Abstract The enhanced warming of the Arctic, relative to other parts of the Earth, a phenomenon known as Arctic amplification, is one of the most striking features of climate change, and has important climatic impacts for the entire Northern Hemisphere. Several mechanisms are believed to be responsible for Arctic amplification; however, a quantitative understanding of their relative importance is still missing. Here, using ensembles of model integrations, we quantify the contribution of ocean coupling, both its thermodynamic and dynamic components, to Arctic amplification over the 20th and 21st centuries. We show that ocean coupling accounts for ~80% of the amplification by 2100. In particular, we show that thermodynamic coupling is responsible for future amplification and sea-ice loss as it overcomes the effect of dynamic coupling which reduces the amplification and sea-ice loss by ~35%. Our results demonstrate the utility of targeted numerical experiments to quantify the role of specific mechanisms in Arctic amplification, for better constraining climate projections. |
format |
article |
author |
Rei Chemke Lorenzo M. Polvani Jennifer E. Kay Clara Orbe |
author_facet |
Rei Chemke Lorenzo M. Polvani Jennifer E. Kay Clara Orbe |
author_sort |
Rei Chemke |
title |
Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century |
title_short |
Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century |
title_full |
Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century |
title_fullStr |
Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century |
title_full_unstemmed |
Quantifying the role of ocean coupling in Arctic amplification and sea-ice loss over the 21st century |
title_sort |
quantifying the role of ocean coupling in arctic amplification and sea-ice loss over the 21st century |
publisher |
Nature Portfolio |
publishDate |
2021 |
url |
https://doaj.org/article/61048e2ffade48e78ba570dc1492ca84 |
work_keys_str_mv |
AT reichemke quantifyingtheroleofoceancouplinginarcticamplificationandseaicelossoverthe21stcentury AT lorenzompolvani quantifyingtheroleofoceancouplinginarcticamplificationandseaicelossoverthe21stcentury AT jenniferekay quantifyingtheroleofoceancouplinginarcticamplificationandseaicelossoverthe21stcentury AT claraorbe quantifyingtheroleofoceancouplinginarcticamplificationandseaicelossoverthe21stcentury |
_version_ |
1718376973556776960 |