Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China
Abstract Stable-oxygen-isotope ratios (δ 18 O) of precipitation and ice-core samples collected from the headwaters of the Urümqi river, Tien Shan, China, were used to test the relationship between δ 18 O and contemporaneous surface air temperature (T a ). A strong temporal relationship is found betw...
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crcambridgeupr:10.1017/s0022143000001374 2024-03-03T08:45:21+00:00 Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China Shugui, Hou Dahe, Qin Mayewski, Paul A. Qinzhao, Yang Jiawen, Ren Zhongqin, Li Cunde, Xiao 1999 http://dx.doi.org/10.1017/s0022143000001374 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001374 en eng Cambridge University Press (CUP) Journal of Glaciology volume 45, issue 151, page 517-523 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1999 crcambridgeupr https://doi.org/10.1017/s0022143000001374 2024-02-08T08:40:37Z Abstract Stable-oxygen-isotope ratios (δ 18 O) of precipitation and ice-core samples collected from the headwaters of the Urümqi river, Tien Shan, China, were used to test the relationship between δ 18 O and contemporaneous surface air temperature (T a ). A strong temporal relationship is found between δ 18 O in precipitation and T a , particularly for the monthly averages which remove synoptic-scale influences such as changes in condensation level, condensation temperature and moisture sources ( Yao and others, 1996). Linear fits as high as 0.95‰° C -1 for precipitation events and 1.23‰° C -1 for monthly averages are found. Although the δ 18 O amplitude in ice cores drilled at the nearby Ürümqi glacier No.1(~2 km from the precipitation sampling site) decreased dramatically compared to the precipitation samples, the ice-core records of annually averaged δ 18 are still positively correlated with contemporaneous air temperature, especially summer air temperature, at the nearby Daxigou meteorological station. Nevertheless, the relationship between the ice-core δ 18 O records and contemporaneous air temperature is less significant than that for the precipitation samples due to depositional and post-depositional modification processes, which are highlighted by the successive snow-pit δ 18 O profiles from the Ürümqi glacier No.1. Our results might extend the application of high-altitude and subtropical ice-core δ 18 O — T a records for paleoclimate reconstruction. Article in Journal/Newspaper ice core Journal of Glaciology Cambridge University Press Journal of Glaciology 45 151 517 523 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Shugui, Hou Dahe, Qin Mayewski, Paul A. Qinzhao, Yang Jiawen, Ren Zhongqin, Li Cunde, Xiao Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China |
topic_facet |
Earth-Surface Processes |
description |
Abstract Stable-oxygen-isotope ratios (δ 18 O) of precipitation and ice-core samples collected from the headwaters of the Urümqi river, Tien Shan, China, were used to test the relationship between δ 18 O and contemporaneous surface air temperature (T a ). A strong temporal relationship is found between δ 18 O in precipitation and T a , particularly for the monthly averages which remove synoptic-scale influences such as changes in condensation level, condensation temperature and moisture sources ( Yao and others, 1996). Linear fits as high as 0.95‰° C -1 for precipitation events and 1.23‰° C -1 for monthly averages are found. Although the δ 18 O amplitude in ice cores drilled at the nearby Ürümqi glacier No.1(~2 km from the precipitation sampling site) decreased dramatically compared to the precipitation samples, the ice-core records of annually averaged δ 18 are still positively correlated with contemporaneous air temperature, especially summer air temperature, at the nearby Daxigou meteorological station. Nevertheless, the relationship between the ice-core δ 18 O records and contemporaneous air temperature is less significant than that for the precipitation samples due to depositional and post-depositional modification processes, which are highlighted by the successive snow-pit δ 18 O profiles from the Ürümqi glacier No.1. Our results might extend the application of high-altitude and subtropical ice-core δ 18 O — T a records for paleoclimate reconstruction. |
format |
Article in Journal/Newspaper |
author |
Shugui, Hou Dahe, Qin Mayewski, Paul A. Qinzhao, Yang Jiawen, Ren Zhongqin, Li Cunde, Xiao |
author_facet |
Shugui, Hou Dahe, Qin Mayewski, Paul A. Qinzhao, Yang Jiawen, Ren Zhongqin, Li Cunde, Xiao |
author_sort |
Shugui, Hou |
title |
Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China |
title_short |
Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China |
title_full |
Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China |
title_fullStr |
Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China |
title_full_unstemmed |
Climatological significance of δ18 O in precipitation and ice cores: a case study at the head of the Ürümqi river, Tien Shan, China |
title_sort |
climatological significance of δ18 o in precipitation and ice cores: a case study at the head of the ürümqi river, tien shan, china |
publisher |
Cambridge University Press (CUP) |
publishDate |
1999 |
url |
http://dx.doi.org/10.1017/s0022143000001374 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001374 |
genre |
ice core Journal of Glaciology |
genre_facet |
ice core Journal of Glaciology |
op_source |
Journal of Glaciology volume 45, issue 151, page 517-523 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000001374 |
container_title |
Journal of Glaciology |
container_volume |
45 |
container_issue |
151 |
container_start_page |
517 |
op_container_end_page |
523 |
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1792500886668312576 |