The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica

Recent studies have suggested that water isotopologues in snow pits from remote East Antarctica can be influenced by the input of stratospheric water, which has anomalously high 17O-excess values. However, it remains unclear whether the 17O-excess records preserved in snow and ice from this region c...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Pang, Hongxi, Zhang, Peng, Wu, Shuangye, Jouzel, Jean, Steen-Larsen, Hans Christian, Liu, Ke, Zhang, Wangbin, Yu, Jinhai, An, Chunlei, Chen, Deliang, Hou, Shugui
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2022
Subjects:
Online Access:https://hdl.handle.net/11250/3026578
https://doi.org/10.1029/2022JD036559
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spelling ftunivbergen:oai:bora.uib.no:11250/3026578 2023-05-15T13:53:35+02:00 The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica Pang, Hongxi Zhang, Peng Wu, Shuangye Jouzel, Jean Steen-Larsen, Hans Christian Liu, Ke Zhang, Wangbin Yu, Jinhai An, Chunlei Chen, Deliang Hou, Shugui 2022 application/pdf https://hdl.handle.net/11250/3026578 https://doi.org/10.1029/2022JD036559 eng eng American Geophysical Union urn:issn:2169-897X https://hdl.handle.net/11250/3026578 https://doi.org/10.1029/2022JD036559 cristin:2058171 Journal of Geophysical Research (JGR): Atmospheres. 2022, 127 (13), e2022JD036559. Copyright 2022 American Geophysical Union. All Rights Reserved. e2022JD036559 Journal of Geophysical Research (JGR): Atmospheres 127 13 Journal article Peer reviewed 2022 ftunivbergen https://doi.org/10.1029/2022JD036559 2023-03-14T17:40:53Z Recent studies have suggested that water isotopologues in snow pits from remote East Antarctica can be influenced by the input of stratospheric water, which has anomalously high 17O-excess values. However, it remains unclear whether the 17O-excess records preserved in snow and ice from this region can be used to reconstruct stratosphere-troposphere exchange (STE). In this study, we present high-resolution 17O-excess records from two snow pits at Dome A, the highest point of the Antarctic ice sheet. The 17O-excess records show a significant positive correlation with the strength of the Brewer-Dobson circulation (BDC), the hemispheric-scale troposphere-stratosphere overturn circulation. Stronger BDC leads to more stratospheric water input over Antarctica and higher 17O-excess, and vice versa. In addition, the 17O-excess records also have a significant positive correlation with the Southern Annular Mode (SAM) index, because SAM modulates Antarctic precipitation, which has a dilution effect on the stratospheric water input. The 17O-excess records do not show significant correlations with local temperature and relative humidity in the moisture source region. These results suggest the dominant effect of BDC on 17O-excess and indicate the potential for using 17O-excess records in ice cores from remote sites in East Antarctica for reconstructing long-term variations of STE, and understanding their mechanisms and climate effects. publishedVersion Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet University of Bergen: Bergen Open Research Archive (BORA-UiB) Antarctic East Antarctica The Antarctic Journal of Geophysical Research: Atmospheres 127 13
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description Recent studies have suggested that water isotopologues in snow pits from remote East Antarctica can be influenced by the input of stratospheric water, which has anomalously high 17O-excess values. However, it remains unclear whether the 17O-excess records preserved in snow and ice from this region can be used to reconstruct stratosphere-troposphere exchange (STE). In this study, we present high-resolution 17O-excess records from two snow pits at Dome A, the highest point of the Antarctic ice sheet. The 17O-excess records show a significant positive correlation with the strength of the Brewer-Dobson circulation (BDC), the hemispheric-scale troposphere-stratosphere overturn circulation. Stronger BDC leads to more stratospheric water input over Antarctica and higher 17O-excess, and vice versa. In addition, the 17O-excess records also have a significant positive correlation with the Southern Annular Mode (SAM) index, because SAM modulates Antarctic precipitation, which has a dilution effect on the stratospheric water input. The 17O-excess records do not show significant correlations with local temperature and relative humidity in the moisture source region. These results suggest the dominant effect of BDC on 17O-excess and indicate the potential for using 17O-excess records in ice cores from remote sites in East Antarctica for reconstructing long-term variations of STE, and understanding their mechanisms and climate effects. publishedVersion
format Article in Journal/Newspaper
author Pang, Hongxi
Zhang, Peng
Wu, Shuangye
Jouzel, Jean
Steen-Larsen, Hans Christian
Liu, Ke
Zhang, Wangbin
Yu, Jinhai
An, Chunlei
Chen, Deliang
Hou, Shugui
spellingShingle Pang, Hongxi
Zhang, Peng
Wu, Shuangye
Jouzel, Jean
Steen-Larsen, Hans Christian
Liu, Ke
Zhang, Wangbin
Yu, Jinhai
An, Chunlei
Chen, Deliang
Hou, Shugui
The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica
author_facet Pang, Hongxi
Zhang, Peng
Wu, Shuangye
Jouzel, Jean
Steen-Larsen, Hans Christian
Liu, Ke
Zhang, Wangbin
Yu, Jinhai
An, Chunlei
Chen, Deliang
Hou, Shugui
author_sort Pang, Hongxi
title The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica
title_short The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica
title_full The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica
title_fullStr The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica
title_full_unstemmed The Dominant Role of Brewer-Dobson Circulation on 17O-Excess Variations in Snow Pits at Dome A, Antarctica
title_sort dominant role of brewer-dobson circulation on 17o-excess variations in snow pits at dome a, antarctica
publisher American Geophysical Union
publishDate 2022
url https://hdl.handle.net/11250/3026578
https://doi.org/10.1029/2022JD036559
geographic Antarctic
East Antarctica
The Antarctic
geographic_facet Antarctic
East Antarctica
The Antarctic
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
op_source e2022JD036559
Journal of Geophysical Research (JGR): Atmospheres
127
13
op_relation urn:issn:2169-897X
https://hdl.handle.net/11250/3026578
https://doi.org/10.1029/2022JD036559
cristin:2058171
Journal of Geophysical Research (JGR): Atmospheres. 2022, 127 (13), e2022JD036559.
op_rights Copyright 2022 American Geophysical Union. All Rights Reserved.
op_doi https://doi.org/10.1029/2022JD036559
container_title Journal of Geophysical Research: Atmospheres
container_volume 127
container_issue 13
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