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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Online Access: | https://hdl.handle.net/11250/3026578 https://doi.org/10.1029/2022JD036559 |
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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 |
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Open Polar |
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University of Bergen: Bergen Open Research Archive (BORA-UiB) |
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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 |
_version_ |
1766258780338651136 |