The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes
Stratigraphic variations of oxygen isotopes in the snow which accumulates during the winter at the Norwegian glacier Austre Okstindbreen are not entirely eliminated after 1-2 months of ablation in the following summer. The relationship between regional temperature changes and δ 18O values in the sno...
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ftumanchesterpub:oai:pure.atira.dk:publications/6e638967-80f3-4d16-85bc-a5902acc0752 2023-11-12T04:19:55+01:00 The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes Yuanqing, H. Theakstone, W. H. Tandong, Y. Yafeng, S. 2001 https://research.manchester.ac.uk/en/publications/6e638967-80f3-4d16-85bc-a5902acc0752 eng eng info:eu-repo/semantics/restrictedAccess Yuanqing , H , Theakstone , W H , Tandong , Y & Yafeng , S 2001 , ' The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes ' , Journal of Glaciology , vol. 47 , no. 156 , pp. 147-151 . article 2001 ftumanchesterpub 2023-10-30T09:14:34Z Stratigraphic variations of oxygen isotopes in the snow which accumulates during the winter at the Norwegian glacier Austre Okstindbreen are not entirely eliminated after 1-2 months of ablation in the following summer. The relationship between regional temperature changes and δ 18O values in the snowpack is affected by many natural factors, but 1989/90 winter air temperatures were reflected in the snow which remained on Austre Okstindbreen at 1350 m a.s.l. in July 1990. There were many variations of δ 18O values in the 4.1m of snow above the 1989 summer surface, but variations in the underlying firn were relatively small. Meltwater percolation modifies the initial variations of δ 18O values in the snowpack. At a site below the mean equilibrium-line altitude on Austre Okstindbreen, increased isotopic homogenization within a 10 day period in July accompanied an increase of the mean δ 18O value. Although the isotopic record at a temperate glacier is likely to be influenced by more factors than is that at polar glaciers, it can provide an estimate of the approximate trend of local temperature variations. Article in Journal/Newspaper Journal of Glaciology The University of Manchester: Research Explorer austre Okstindbreen ENVELOPE(14.293,14.293,66.014,66.014) Okstindbreen ENVELOPE(14.148,14.148,65.987,65.987) |
institution |
Open Polar |
collection |
The University of Manchester: Research Explorer |
op_collection_id |
ftumanchesterpub |
language |
English |
description |
Stratigraphic variations of oxygen isotopes in the snow which accumulates during the winter at the Norwegian glacier Austre Okstindbreen are not entirely eliminated after 1-2 months of ablation in the following summer. The relationship between regional temperature changes and δ 18O values in the snowpack is affected by many natural factors, but 1989/90 winter air temperatures were reflected in the snow which remained on Austre Okstindbreen at 1350 m a.s.l. in July 1990. There were many variations of δ 18O values in the 4.1m of snow above the 1989 summer surface, but variations in the underlying firn were relatively small. Meltwater percolation modifies the initial variations of δ 18O values in the snowpack. At a site below the mean equilibrium-line altitude on Austre Okstindbreen, increased isotopic homogenization within a 10 day period in July accompanied an increase of the mean δ 18O value. Although the isotopic record at a temperate glacier is likely to be influenced by more factors than is that at polar glaciers, it can provide an estimate of the approximate trend of local temperature variations. |
format |
Article in Journal/Newspaper |
author |
Yuanqing, H. Theakstone, W. H. Tandong, Y. Yafeng, S. |
spellingShingle |
Yuanqing, H. Theakstone, W. H. Tandong, Y. Yafeng, S. The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes |
author_facet |
Yuanqing, H. Theakstone, W. H. Tandong, Y. Yafeng, S. |
author_sort |
Yuanqing, H. |
title |
The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes |
title_short |
The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes |
title_full |
The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes |
title_fullStr |
The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes |
title_full_unstemmed |
The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes |
title_sort |
isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes |
publishDate |
2001 |
url |
https://research.manchester.ac.uk/en/publications/6e638967-80f3-4d16-85bc-a5902acc0752 |
long_lat |
ENVELOPE(14.293,14.293,66.014,66.014) ENVELOPE(14.148,14.148,65.987,65.987) |
geographic |
austre Okstindbreen Okstindbreen |
geographic_facet |
austre Okstindbreen Okstindbreen |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Yuanqing , H , Theakstone , W H , Tandong , Y & Yafeng , S 2001 , ' The isotopic record at an alpine glacier and its implications for local climatic changes and isotopic homogenization processes ' , Journal of Glaciology , vol. 47 , no. 156 , pp. 147-151 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1782336145143627776 |