Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year

Abstract Warming has been and is being enhanced at high latitudes or high elevations, whereas the quantitative estimation for warming from altitude and latitude effects has not been systematically investigated over Antarctic Ice Sheet, which covers more than 27 degrees of latitude and 4000 m altitud...

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Published in:Scientific Reports
Main Authors: Aihong Xie, Jiangping Zhu, Xiang Qin, Shimeng Wang, Bing Xu, Yicheng Wang
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
R
Q
Online Access:https://doi.org/10.1038/s41598-023-35521-w
https://doaj.org/article/6f45e952bbc44546b74b4a4802664d0c
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spelling ftdoajarticles:oai:doaj.org/article:6f45e952bbc44546b74b4a4802664d0c 2023-07-16T03:52:20+02:00 Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year Aihong Xie Jiangping Zhu Xiang Qin Shimeng Wang Bing Xu Yicheng Wang 2023-06-01T00:00:00Z https://doi.org/10.1038/s41598-023-35521-w https://doaj.org/article/6f45e952bbc44546b74b4a4802664d0c EN eng Nature Portfolio https://doi.org/10.1038/s41598-023-35521-w https://doaj.org/toc/2045-2322 doi:10.1038/s41598-023-35521-w 2045-2322 https://doaj.org/article/6f45e952bbc44546b74b4a4802664d0c Scientific Reports, Vol 13, Iss 1, Pp 1-11 (2023) Medicine R Science Q article 2023 ftdoajarticles https://doi.org/10.1038/s41598-023-35521-w 2023-06-25T00:37:27Z Abstract Warming has been and is being enhanced at high latitudes or high elevations, whereas the quantitative estimation for warming from altitude and latitude effects has not been systematically investigated over Antarctic Ice Sheet, which covers more than 27 degrees of latitude and 4000 m altitude ranges. Based on the monthly surface air temperature data (1958–2020) from ERA5 reanalysis, this work aims to explore whether elevation-dependent warming (EDW) and latitude-dependent warming (LDW) exist. Results show that both EDW and LDW have the cooperative effect on Antarctic warming, and the magnitude of EDW is stronger than LDW. The negative EDW appears between 250 m and 2500 m except winter, and is strongest in autumn. The negative LDW occurs between 83 °S and 90 °S except in summer. Moreover, the surface downward long-wave radiation that related to the specific humidity, total cloud cover and cloud base height is a major contributor to the EDW over Antarctica. Further research on EDW and LDW should be anticipated to explore the future Antarctic amplification under different emission scenarios. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Directory of Open Access Journals: DOAJ Articles Antarctic Scientific Reports 13 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Aihong Xie
Jiangping Zhu
Xiang Qin
Shimeng Wang
Bing Xu
Yicheng Wang
Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year
topic_facet Medicine
R
Science
Q
description Abstract Warming has been and is being enhanced at high latitudes or high elevations, whereas the quantitative estimation for warming from altitude and latitude effects has not been systematically investigated over Antarctic Ice Sheet, which covers more than 27 degrees of latitude and 4000 m altitude ranges. Based on the monthly surface air temperature data (1958–2020) from ERA5 reanalysis, this work aims to explore whether elevation-dependent warming (EDW) and latitude-dependent warming (LDW) exist. Results show that both EDW and LDW have the cooperative effect on Antarctic warming, and the magnitude of EDW is stronger than LDW. The negative EDW appears between 250 m and 2500 m except winter, and is strongest in autumn. The negative LDW occurs between 83 °S and 90 °S except in summer. Moreover, the surface downward long-wave radiation that related to the specific humidity, total cloud cover and cloud base height is a major contributor to the EDW over Antarctica. Further research on EDW and LDW should be anticipated to explore the future Antarctic amplification under different emission scenarios.
format Article in Journal/Newspaper
author Aihong Xie
Jiangping Zhu
Xiang Qin
Shimeng Wang
Bing Xu
Yicheng Wang
author_facet Aihong Xie
Jiangping Zhu
Xiang Qin
Shimeng Wang
Bing Xu
Yicheng Wang
author_sort Aihong Xie
title Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year
title_short Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year
title_full Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year
title_fullStr Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year
title_full_unstemmed Surface warming from altitudinal and latitudinal amplification over Antarctica since the International Geophysical Year
title_sort surface warming from altitudinal and latitudinal amplification over antarctica since the international geophysical year
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41598-023-35521-w
https://doaj.org/article/6f45e952bbc44546b74b4a4802664d0c
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_source Scientific Reports, Vol 13, Iss 1, Pp 1-11 (2023)
op_relation https://doi.org/10.1038/s41598-023-35521-w
https://doaj.org/toc/2045-2322
doi:10.1038/s41598-023-35521-w
2045-2322
https://doaj.org/article/6f45e952bbc44546b74b4a4802664d0c
op_doi https://doi.org/10.1038/s41598-023-35521-w
container_title Scientific Reports
container_volume 13
container_issue 1
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