Validation of reanalysis Southern Ocean atmosphere trends using sea ice data

Reanalysis products are an invaluable tool for representing variability and long-term trends in regions with limited in situ data, and especially the Antarctic. A comparison of eight different reanalysis products shows large differences in sea level pressure and surface air temperature trends over t...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Hobbs, WR, Klekociuk, AR, Pan, Y
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2020
Subjects:
Online Access:https://eprints.utas.edu.au/44058/
https://eprints.utas.edu.au/44058/1/141922%20-%20Validation%20of%20reanalysis%20Southern%20Ocean%20atmosphere%20trends%20using%20sea%20ice%20data.pdf
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spelling ftunivtasmania:oai:eprints.utas.edu.au:44058 2023-05-15T13:41:50+02:00 Validation of reanalysis Southern Ocean atmosphere trends using sea ice data Hobbs, WR Klekociuk, AR Pan, Y 2020 application/pdf https://eprints.utas.edu.au/44058/ https://eprints.utas.edu.au/44058/1/141922%20-%20Validation%20of%20reanalysis%20Southern%20Ocean%20atmosphere%20trends%20using%20sea%20ice%20data.pdf en eng Copernicus GmbH https://eprints.utas.edu.au/44058/1/141922%20-%20Validation%20of%20reanalysis%20Southern%20Ocean%20atmosphere%20trends%20using%20sea%20ice%20data.pdf Hobbs, WR orcid:0000-0002-2061-0899 , Klekociuk, AR and Pan, Y 2020 , 'Validation of reanalysis Southern Ocean atmosphere trends using sea ice data' , Atmospheric Chemistry and Physics, vol. 20 , 14757–14768 , doi:10.5194/acp-20-14757-2020 <http://dx.doi.org/10.5194/acp-20-14757-2020>. Southern Ocean trends atmosphere Article PeerReviewed 2020 ftunivtasmania https://doi.org/10.5194/acp-20-14757-2020 2022-02-28T23:16:41Z Reanalysis products are an invaluable tool for representing variability and long-term trends in regions with limited in situ data, and especially the Antarctic. A comparison of eight different reanalysis products shows large differences in sea level pressure and surface air temperature trends over the high-latitude Southern Ocean, with implications for studies of the atmosphere's role in driving ocean–sea ice changes. In this study, we use the established close coupling between sea ice cover and surface temperature to evaluate these reanalysis trends using the independent, 30-year sea ice record from 1980 to 2010. We demonstrate that sea ice trends are a reliable validation tool for most months of the year, although the sea ice–surface temperature coupling is weakest in summer when the surface energy budget is dominated by atmosphere-to-ocean heat fluxes. Based on our analysis, we find that surface air temperature trends in JRA55 are most consistent with satellite-observed sea ice trends over the polar waters of the Southern Ocean. Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean University of Tasmania: UTas ePrints Antarctic Southern Ocean The Antarctic Atmospheric Chemistry and Physics 20 23 14757 14768
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic Southern Ocean
trends
atmosphere
spellingShingle Southern Ocean
trends
atmosphere
Hobbs, WR
Klekociuk, AR
Pan, Y
Validation of reanalysis Southern Ocean atmosphere trends using sea ice data
topic_facet Southern Ocean
trends
atmosphere
description Reanalysis products are an invaluable tool for representing variability and long-term trends in regions with limited in situ data, and especially the Antarctic. A comparison of eight different reanalysis products shows large differences in sea level pressure and surface air temperature trends over the high-latitude Southern Ocean, with implications for studies of the atmosphere's role in driving ocean–sea ice changes. In this study, we use the established close coupling between sea ice cover and surface temperature to evaluate these reanalysis trends using the independent, 30-year sea ice record from 1980 to 2010. We demonstrate that sea ice trends are a reliable validation tool for most months of the year, although the sea ice–surface temperature coupling is weakest in summer when the surface energy budget is dominated by atmosphere-to-ocean heat fluxes. Based on our analysis, we find that surface air temperature trends in JRA55 are most consistent with satellite-observed sea ice trends over the polar waters of the Southern Ocean.
format Article in Journal/Newspaper
author Hobbs, WR
Klekociuk, AR
Pan, Y
author_facet Hobbs, WR
Klekociuk, AR
Pan, Y
author_sort Hobbs, WR
title Validation of reanalysis Southern Ocean atmosphere trends using sea ice data
title_short Validation of reanalysis Southern Ocean atmosphere trends using sea ice data
title_full Validation of reanalysis Southern Ocean atmosphere trends using sea ice data
title_fullStr Validation of reanalysis Southern Ocean atmosphere trends using sea ice data
title_full_unstemmed Validation of reanalysis Southern Ocean atmosphere trends using sea ice data
title_sort validation of reanalysis southern ocean atmosphere trends using sea ice data
publisher Copernicus GmbH
publishDate 2020
url https://eprints.utas.edu.au/44058/
https://eprints.utas.edu.au/44058/1/141922%20-%20Validation%20of%20reanalysis%20Southern%20Ocean%20atmosphere%20trends%20using%20sea%20ice%20data.pdf
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_relation https://eprints.utas.edu.au/44058/1/141922%20-%20Validation%20of%20reanalysis%20Southern%20Ocean%20atmosphere%20trends%20using%20sea%20ice%20data.pdf
Hobbs, WR orcid:0000-0002-2061-0899 , Klekociuk, AR and Pan, Y 2020 , 'Validation of reanalysis Southern Ocean atmosphere trends using sea ice data' , Atmospheric Chemistry and Physics, vol. 20 , 14757–14768 , doi:10.5194/acp-20-14757-2020 <http://dx.doi.org/10.5194/acp-20-14757-2020>.
op_doi https://doi.org/10.5194/acp-20-14757-2020
container_title Atmospheric Chemistry and Physics
container_volume 20
container_issue 23
container_start_page 14757
op_container_end_page 14768
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