Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols

The North Atlantic Warming Hole (NAWH) has been observed and predicted due to the increase in carbon dioxide (CO(2)) concentration. If sulphate aerosols, which have a cooling effect on the atmosphere, are reduced by air pollution control, the NAWH may form as it would if CO(2) concentrations increas...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Kusakabe, Yuki, Takemura, Toshihiko
Format: Text
Language:English
Published: Nature Publishing Group UK 2023
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9807570/
http://www.ncbi.nlm.nih.gov/pubmed/36593248
https://doi.org/10.1038/s41598-022-27315-3
id ftpubmed:oai:pubmedcentral.nih.gov:9807570
record_format openpolar
spelling ftpubmed:oai:pubmedcentral.nih.gov:9807570 2023-05-15T15:06:56+02:00 Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols Kusakabe, Yuki Takemura, Toshihiko 2023-01-02 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9807570/ http://www.ncbi.nlm.nih.gov/pubmed/36593248 https://doi.org/10.1038/s41598-022-27315-3 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9807570/ http://www.ncbi.nlm.nih.gov/pubmed/36593248 http://dx.doi.org/10.1038/s41598-022-27315-3 © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . CC-BY Sci Rep Article Text 2023 ftpubmed https://doi.org/10.1038/s41598-022-27315-3 2023-01-08T02:07:17Z The North Atlantic Warming Hole (NAWH) has been observed and predicted due to the increase in carbon dioxide (CO(2)) concentration. If sulphate aerosols, which have a cooling effect on the atmosphere, are reduced by air pollution control, the NAWH may form as it would if CO(2) concentrations increased. In this study, sensitivity experiments using a coupled atmosphere–ocean-aerosol model were conducted by varying the amount of sulphur dioxide (SO(2)) emissions, a precursor of sulphate which is the primary anthropogenic aerosol in the atmosphere, to analyse the changes in the ocean temperature, salinity, and density. The results showed that although the spatial patterns of the NAWH due to the changes in SO(2) emissions was similar to that due to the changes in the CO(2) concentrations, the magnitude of the shifts in the ocean parameters due to the changes in SO(2) emissions is larger even when changes in global mean temperature are comparable. This can be due to the spatial concentration of sulphate aerosols in the mid-latitudes of the Northern Hemisphere, resulting larger changes in the heat transport from the south on the Gulf Stream and the North Atlantic Current along with changes in freshwater inflow from the Arctic through the Labrador Sea. Text Arctic Labrador Sea north atlantic current North Atlantic PubMed Central (PMC) Arctic Scientific Reports 13 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Kusakabe, Yuki
Takemura, Toshihiko
Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols
topic_facet Article
description The North Atlantic Warming Hole (NAWH) has been observed and predicted due to the increase in carbon dioxide (CO(2)) concentration. If sulphate aerosols, which have a cooling effect on the atmosphere, are reduced by air pollution control, the NAWH may form as it would if CO(2) concentrations increased. In this study, sensitivity experiments using a coupled atmosphere–ocean-aerosol model were conducted by varying the amount of sulphur dioxide (SO(2)) emissions, a precursor of sulphate which is the primary anthropogenic aerosol in the atmosphere, to analyse the changes in the ocean temperature, salinity, and density. The results showed that although the spatial patterns of the NAWH due to the changes in SO(2) emissions was similar to that due to the changes in the CO(2) concentrations, the magnitude of the shifts in the ocean parameters due to the changes in SO(2) emissions is larger even when changes in global mean temperature are comparable. This can be due to the spatial concentration of sulphate aerosols in the mid-latitudes of the Northern Hemisphere, resulting larger changes in the heat transport from the south on the Gulf Stream and the North Atlantic Current along with changes in freshwater inflow from the Arctic through the Labrador Sea.
format Text
author Kusakabe, Yuki
Takemura, Toshihiko
author_facet Kusakabe, Yuki
Takemura, Toshihiko
author_sort Kusakabe, Yuki
title Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols
title_short Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols
title_full Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols
title_fullStr Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols
title_full_unstemmed Formation of the North Atlantic Warming Hole by reducing anthropogenic sulphate aerosols
title_sort formation of the north atlantic warming hole by reducing anthropogenic sulphate aerosols
publisher Nature Publishing Group UK
publishDate 2023
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9807570/
http://www.ncbi.nlm.nih.gov/pubmed/36593248
https://doi.org/10.1038/s41598-022-27315-3
geographic Arctic
geographic_facet Arctic
genre Arctic
Labrador Sea
north atlantic current
North Atlantic
genre_facet Arctic
Labrador Sea
north atlantic current
North Atlantic
op_source Sci Rep
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9807570/
http://www.ncbi.nlm.nih.gov/pubmed/36593248
http://dx.doi.org/10.1038/s41598-022-27315-3
op_rights © The Author(s) 2023
https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/s41598-022-27315-3
container_title Scientific Reports
container_volume 13
container_issue 1
_version_ 1766338521872728064