Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note)
The stable oxygen isotope ratio (δ^<18>O) in ice cores and surface snow pits samples obtained in Svalbard does not show a seasonal variation clearly. In preceding research, it has been reported that δ^<18>O is change by melting of the snow layer. However, to what degree δ^<18>O in...
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National Institute of Polar Research
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ftnipr:oai:nipr.repo.nii.ac.jp:00002372 2023-05-15T16:39:20+02:00 Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note) Makoto Igarashi Kokichi Kamiyama Okitsugu Watanabe 2001-03 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2372 http://id.nii.ac.jp/1291/00002372/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2372&item_no=1&attribute_id=18&file_no=1 en eng National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2372 http://id.nii.ac.jp/1291/00002372/ AA00733561 Memoirs of National Institute of Polar Research. Special issue, 54, 169-182(2001-03) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2372&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 2001 ftnipr 2022-11-12T19:43:08Z The stable oxygen isotope ratio (δ^<18>O) in ice cores and surface snow pits samples obtained in Svalbard does not show a seasonal variation clearly. In preceding research, it has been reported that δ^<18>O is change by melting of the snow layer. However, to what degree δ^<18>O in snow changes after accumulation is not clear. We carried out the observation in Ny-Ålesund, northwestern part of Svalbard, in the 1993/94 winter season and 1994 summer season in order to investigate the initial values of δ^<18>O in precipitations. Values of δ^<18>O both in winter and summer were almost same (-4∿-24‰) as well as the average of each season was also almost same (-12.9‰, -12.3‰), which shows that δ^<18>O in precipitations does not have a clear seasonal variation. It is known that the value of δ^<18>O in precipitation changes by the condensation temperature of water vapor. Temperature, at the height where the wettest air mass existed over northwestern Svalbard, changed almost same range in winter and summer, when the rain fell at Ny-Ålesund. And, there was a better correlation between δ^<18>O in precipitation and temperature of moist air masses than δ^<18>O in precipitation and air temperature at the observation site both in winter and in summer. Therefore, fluctuation of δ^<18>O seemed to show the almost equal, even if the season was different. This fact can be regarded that one of the reasons why δ^<18>O of ice core drilled in Svalbard does not show the seasonal variation clearly. Report ice core Memoirs of National Institute of Polar Research Ny Ålesund Ny-Ålesund Polar Research Svalbard National Institute of Polar Research Repository, Japan Ny-Ålesund Svalbard |
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National Institute of Polar Research Repository, Japan |
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English |
description |
The stable oxygen isotope ratio (δ^<18>O) in ice cores and surface snow pits samples obtained in Svalbard does not show a seasonal variation clearly. In preceding research, it has been reported that δ^<18>O is change by melting of the snow layer. However, to what degree δ^<18>O in snow changes after accumulation is not clear. We carried out the observation in Ny-Ålesund, northwestern part of Svalbard, in the 1993/94 winter season and 1994 summer season in order to investigate the initial values of δ^<18>O in precipitations. Values of δ^<18>O both in winter and summer were almost same (-4∿-24‰) as well as the average of each season was also almost same (-12.9‰, -12.3‰), which shows that δ^<18>O in precipitations does not have a clear seasonal variation. It is known that the value of δ^<18>O in precipitation changes by the condensation temperature of water vapor. Temperature, at the height where the wettest air mass existed over northwestern Svalbard, changed almost same range in winter and summer, when the rain fell at Ny-Ålesund. And, there was a better correlation between δ^<18>O in precipitation and temperature of moist air masses than δ^<18>O in precipitation and air temperature at the observation site both in winter and in summer. Therefore, fluctuation of δ^<18>O seemed to show the almost equal, even if the season was different. This fact can be regarded that one of the reasons why δ^<18>O of ice core drilled in Svalbard does not show the seasonal variation clearly. |
format |
Report |
author |
Makoto Igarashi Kokichi Kamiyama Okitsugu Watanabe |
spellingShingle |
Makoto Igarashi Kokichi Kamiyama Okitsugu Watanabe Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note) |
author_facet |
Makoto Igarashi Kokichi Kamiyama Okitsugu Watanabe |
author_sort |
Makoto Igarashi |
title |
Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note) |
title_short |
Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note) |
title_full |
Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note) |
title_fullStr |
Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note) |
title_full_unstemmed |
Stable oxygen isotope ratio observed in the precipitation at Ny-Alesund, Svalbard (scientific note) |
title_sort |
stable oxygen isotope ratio observed in the precipitation at ny-alesund, svalbard (scientific note) |
publisher |
National Institute of Polar Research |
publishDate |
2001 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2372 http://id.nii.ac.jp/1291/00002372/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2372&item_no=1&attribute_id=18&file_no=1 |
geographic |
Ny-Ålesund Svalbard |
geographic_facet |
Ny-Ålesund Svalbard |
genre |
ice core Memoirs of National Institute of Polar Research Ny Ålesund Ny-Ålesund Polar Research Svalbard |
genre_facet |
ice core Memoirs of National Institute of Polar Research Ny Ålesund Ny-Ålesund Polar Research Svalbard |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2372 http://id.nii.ac.jp/1291/00002372/ AA00733561 Memoirs of National Institute of Polar Research. Special issue, 54, 169-182(2001-03) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2372&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766029666557100032 |