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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Main Authors: Makoto Igarashi, Kokichi Kamiyama, Okitsugu Watanabe
Format: Report
Language:English
Published: National Institute of Polar Research 2001
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2372
http://id.nii.ac.jp/1291/00002372/
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spelling 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
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language 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
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