Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature

Polar amplification has been a research focus in climate research in recent decades. However, little attention has been paid to Antarctic amplification (AnA). We have examined the variations in annual and seasonal temperature over the Antarctic Ice Sheet and its amplification based on reconstruction...

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Published in:Atmosphere
Main Authors: Jiangping Zhu, Aihong Xie, Xiang Qin, Bing Xu, Yicheng Wang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/atmos14020218
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spelling ftmdpi:oai:mdpi.com:/2073-4433/14/2/218/ 2023-08-20T04:01:55+02:00 Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature Jiangping Zhu Aihong Xie Xiang Qin Bing Xu Yicheng Wang agris 2023-01-20 application/pdf https://doi.org/10.3390/atmos14020218 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos14020218 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 2; Pages: 218 Antarctic ice sheet temperature Antarctic amplification reconstruction Text 2023 ftmdpi https://doi.org/10.3390/atmos14020218 2023-08-01T08:24:35Z Polar amplification has been a research focus in climate research in recent decades. However, little attention has been paid to Antarctic amplification (AnA). We have examined the variations in annual and seasonal temperature over the Antarctic Ice Sheet and its amplification based on reconstruction covering the period 2002–2018. The results show the occurrence of annual and seasonal AnA, with an AnA index greater than 1.39 with seasonal differences, and that AnA is strong in the austral winter and spring. Moreover, AnA displays regional differences, with the greatest amplification occurring in East Antarctica, with an AnA index greater than 1.51, followed by West Antarctica. AnA is always absent in the Antarctic Peninsula. In addition, amplification in East Antarctica is most conspicuous in spring, which corresponds to the obvious warming in this season; and the spring amplification signal is weakest for West Antarctica. When considering the influence of the ocean, the AnA becomes obvious, compared to when only the land is considered. Southern Annular Mode (SAM), surface pressure and westerlies work together to affect the temperature change over Antarctica and AnA; and SAM and surface pressure are highly correlated with the temperature change over East Antarctica. The picture reflects the accelerated changes in Antarctic temperature. Text Antarc* Antarctic Antarctic Peninsula Antarctica East Antarctica Ice Sheet West Antarctica MDPI Open Access Publishing Antarctic The Antarctic Antarctic Peninsula East Antarctica Austral West Antarctica Atmosphere 14 2 218
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Antarctic ice sheet
temperature
Antarctic amplification
reconstruction
spellingShingle Antarctic ice sheet
temperature
Antarctic amplification
reconstruction
Jiangping Zhu
Aihong Xie
Xiang Qin
Bing Xu
Yicheng Wang
Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature
topic_facet Antarctic ice sheet
temperature
Antarctic amplification
reconstruction
description Polar amplification has been a research focus in climate research in recent decades. However, little attention has been paid to Antarctic amplification (AnA). We have examined the variations in annual and seasonal temperature over the Antarctic Ice Sheet and its amplification based on reconstruction covering the period 2002–2018. The results show the occurrence of annual and seasonal AnA, with an AnA index greater than 1.39 with seasonal differences, and that AnA is strong in the austral winter and spring. Moreover, AnA displays regional differences, with the greatest amplification occurring in East Antarctica, with an AnA index greater than 1.51, followed by West Antarctica. AnA is always absent in the Antarctic Peninsula. In addition, amplification in East Antarctica is most conspicuous in spring, which corresponds to the obvious warming in this season; and the spring amplification signal is weakest for West Antarctica. When considering the influence of the ocean, the AnA becomes obvious, compared to when only the land is considered. Southern Annular Mode (SAM), surface pressure and westerlies work together to affect the temperature change over Antarctica and AnA; and SAM and surface pressure are highly correlated with the temperature change over East Antarctica. The picture reflects the accelerated changes in Antarctic temperature.
format Text
author Jiangping Zhu
Aihong Xie
Xiang Qin
Bing Xu
Yicheng Wang
author_facet Jiangping Zhu
Aihong Xie
Xiang Qin
Bing Xu
Yicheng Wang
author_sort Jiangping Zhu
title Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature
title_short Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature
title_full Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature
title_fullStr Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature
title_full_unstemmed Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature
title_sort assessment of antarctic amplification based on a reconstruction of near-surface air temperature
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/atmos14020218
op_coverage agris
geographic Antarctic
The Antarctic
Antarctic Peninsula
East Antarctica
Austral
West Antarctica
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
East Antarctica
Austral
West Antarctica
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
Ice Sheet
West Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
Ice Sheet
West Antarctica
op_source Atmosphere; Volume 14; Issue 2; Pages: 218
op_relation Climatology
https://dx.doi.org/10.3390/atmos14020218
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos14020218
container_title Atmosphere
container_volume 14
container_issue 2
container_start_page 218
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