Responses of polar energy budget to regional sea surface temperature changes in extra-polar regions

<p>Surface temperature at polar regions not only is affected by local forcings and feedbacks but also depends on teleconnections between polar regions and low-latitude regions. In this study, the responses of the energy budget in polar regions to remote sea surface temperature (SST) changes ar...

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Main Authors: Q. Wang, Y. Liu, L. Zhang, C. Zhou
Format: Article
Language:English
Published: Copernicus Publications 2025-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/25/6741/2025/acp-25-6741-2025.pdf
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author Q. Wang
Y. Liu
L. Zhang
C. Zhou
author_facet Q. Wang
Y. Liu
L. Zhang
C. Zhou
author_sort Q. Wang
collection DOAJ
description <p>Surface temperature at polar regions not only is affected by local forcings and feedbacks but also depends on teleconnections between polar regions and low-latitude regions. In this study, the responses of the energy budget in polar regions to remote sea surface temperature (SST) changes are analyzed using a set of idealized regional SST perturbation experiments. The results show that the responses of the polar energy budget to remote sea surface warmings are regulated by changes in atmospheric energy transport, and radiative feedbacks also contribute to the polar energy budget at both the top of atmosphere (TOA) and the surface. Specifically, an increase in poleward atmospheric energy transport to polar regions results in an increase in surface and air temperature, and the corresponding Planck feedback leads to radiative warming at the surface and radiative cooling at the TOA. In response to sea surface warmings in most mid-latitude regions, poleward atmospheric energy transport to polar regions in the corresponding hemisphere increases. Sea surface warming over most tropical regions enhances the polar energy transport to both Arctic and Antarctic regions, except that an increase in the Indian Ocean's temperature results in a decrease in poleward atmospheric energy transport to the Arctic due to the different responses of stationary waves. The sensitivity of the Arctic energy budget to tropical SST changes is generally stronger than that of the Antarctic energy budget, and poleward atmospheric heat transport is dominated by dry static energy, with a lesser contribution from latent heat transport. The polar energy budget is not sensitive to SST changes in most subtropical regions. These results help to explain how the polar climate is affected by the magnitude and spatial pattern of remote SST change.</p>
format Article
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issn 1680-7316
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language English
publishDate 2025-07-01
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spelling doaj-art-c8d5f60743354283bafc2b2702b35deb2025-08-20T02:42:15ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242025-07-01256741675510.5194/acp-25-6741-2025Responses of polar energy budget to regional sea surface temperature changes in extra-polar regionsQ. Wang0Y. Liu1L. Zhang2C. Zhou3School of Atmospheric Sciences, Nanjing University, Nanjing, 210023, ChinaSchool of Atmospheric Sciences, Nanjing University, Nanjing, 210023, ChinaSchool of Atmospheric Sciences, Nanjing University, Nanjing, 210023, ChinaSchool of Atmospheric Sciences, Nanjing University, Nanjing, 210023, China<p>Surface temperature at polar regions not only is affected by local forcings and feedbacks but also depends on teleconnections between polar regions and low-latitude regions. In this study, the responses of the energy budget in polar regions to remote sea surface temperature (SST) changes are analyzed using a set of idealized regional SST perturbation experiments. The results show that the responses of the polar energy budget to remote sea surface warmings are regulated by changes in atmospheric energy transport, and radiative feedbacks also contribute to the polar energy budget at both the top of atmosphere (TOA) and the surface. Specifically, an increase in poleward atmospheric energy transport to polar regions results in an increase in surface and air temperature, and the corresponding Planck feedback leads to radiative warming at the surface and radiative cooling at the TOA. In response to sea surface warmings in most mid-latitude regions, poleward atmospheric energy transport to polar regions in the corresponding hemisphere increases. Sea surface warming over most tropical regions enhances the polar energy transport to both Arctic and Antarctic regions, except that an increase in the Indian Ocean's temperature results in a decrease in poleward atmospheric energy transport to the Arctic due to the different responses of stationary waves. The sensitivity of the Arctic energy budget to tropical SST changes is generally stronger than that of the Antarctic energy budget, and poleward atmospheric heat transport is dominated by dry static energy, with a lesser contribution from latent heat transport. The polar energy budget is not sensitive to SST changes in most subtropical regions. These results help to explain how the polar climate is affected by the magnitude and spatial pattern of remote SST change.</p>https://acp.copernicus.org/articles/25/6741/2025/acp-25-6741-2025.pdf
spellingShingle Q. Wang
Y. Liu
L. Zhang
C. Zhou
Responses of polar energy budget to regional sea surface temperature changes in extra-polar regions
Atmospheric Chemistry and Physics
title Responses of polar energy budget to regional sea surface temperature changes in extra-polar regions
title_full Responses of polar energy budget to regional sea surface temperature changes in extra-polar regions
title_fullStr Responses of polar energy budget to regional sea surface temperature changes in extra-polar regions
title_full_unstemmed Responses of polar energy budget to regional sea surface temperature changes in extra-polar regions
title_short Responses of polar energy budget to regional sea surface temperature changes in extra-polar regions
title_sort responses of polar energy budget to regional sea surface temperature changes in extra polar regions
url https://acp.copernicus.org/articles/25/6741/2025/acp-25-6741-2025.pdf
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AT lzhang responsesofpolarenergybudgettoregionalseasurfacetemperaturechangesinextrapolarregions
AT czhou responsesofpolarenergybudgettoregionalseasurfacetemperaturechangesinextrapolarregions