Isotopic mass fractionation of snow due to depth hoar formation
To clarify the isotopic changes (δD and δ^<18>O) of snow due to depth hoar formation, large temperature gradients were imposed on snow samples using a closed and insulated box for several days. δD and δ^<18>O increased in the high temperature region where sublimation enriched heavy H_2O,...
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ftnipr:oai:nipr.repo.nii.ac.jp:00002907 2023-05-15T18:02:10+02:00 Isotopic mass fractionation of snow due to depth hoar formation ハチクボ アキヒロ ハシモト シゲマサ ナカオ マサヨシ ニシムラ コウイチ Akihiro Hachikubo Shigemasa Hashimoto Masayoshi Nakawo Kouichi Nishimura 2000-11 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2907 http://id.nii.ac.jp/1291/00002907/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2907&item_no=1&attribute_id=18&file_no=1 en eng Scientific Paper Kitami Institute of Technology Institute for Hydrospheric-Atmospheric Sciences, Nagoya University Institute of Low Temperature Science, Hokkaido University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2907 http://id.nii.ac.jp/1291/00002907/ AA1129795X Polar meteorology and glaciology, 14, 1-7(2000-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2907&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 2000 ftnipr 2022-11-26T19:42:17Z To clarify the isotopic changes (δD and δ^<18>O) of snow due to depth hoar formation, large temperature gradients were imposed on snow samples using a closed and insulated box for several days. δD and δ^<18>O increased in the high temperature region where sublimation enriched heavy H_2O, and decreased in the low temperature region where light H_2O was concentrated. Isotope diagrams of the data showed slopes of 2.4-4.9,which indicated that isotopic fractionation on sublimation depends on the kinetic isotope effect. It was also suggested that the transfer coefficient of water vapor in snow increases slightly due to convection; and the changes of isotopic profiles depend primary on the snow density as it affects permeability to vapor diffusion. Report Polar meteorology and glaciology National Institute of Polar Research Repository, Japan |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
language |
English |
description |
To clarify the isotopic changes (δD and δ^<18>O) of snow due to depth hoar formation, large temperature gradients were imposed on snow samples using a closed and insulated box for several days. δD and δ^<18>O increased in the high temperature region where sublimation enriched heavy H_2O, and decreased in the low temperature region where light H_2O was concentrated. Isotope diagrams of the data showed slopes of 2.4-4.9,which indicated that isotopic fractionation on sublimation depends on the kinetic isotope effect. It was also suggested that the transfer coefficient of water vapor in snow increases slightly due to convection; and the changes of isotopic profiles depend primary on the snow density as it affects permeability to vapor diffusion. |
format |
Report |
author |
ハチクボ アキヒロ ハシモト シゲマサ ナカオ マサヨシ ニシムラ コウイチ Akihiro Hachikubo Shigemasa Hashimoto Masayoshi Nakawo Kouichi Nishimura |
spellingShingle |
ハチクボ アキヒロ ハシモト シゲマサ ナカオ マサヨシ ニシムラ コウイチ Akihiro Hachikubo Shigemasa Hashimoto Masayoshi Nakawo Kouichi Nishimura Isotopic mass fractionation of snow due to depth hoar formation |
author_facet |
ハチクボ アキヒロ ハシモト シゲマサ ナカオ マサヨシ ニシムラ コウイチ Akihiro Hachikubo Shigemasa Hashimoto Masayoshi Nakawo Kouichi Nishimura |
author_sort |
ハチクボ アキヒロ |
title |
Isotopic mass fractionation of snow due to depth hoar formation |
title_short |
Isotopic mass fractionation of snow due to depth hoar formation |
title_full |
Isotopic mass fractionation of snow due to depth hoar formation |
title_fullStr |
Isotopic mass fractionation of snow due to depth hoar formation |
title_full_unstemmed |
Isotopic mass fractionation of snow due to depth hoar formation |
title_sort |
isotopic mass fractionation of snow due to depth hoar formation |
publisher |
Scientific Paper |
publishDate |
2000 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2907 http://id.nii.ac.jp/1291/00002907/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2907&item_no=1&attribute_id=18&file_no=1 |
genre |
Polar meteorology and glaciology |
genre_facet |
Polar meteorology and glaciology |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2907 http://id.nii.ac.jp/1291/00002907/ AA1129795X Polar meteorology and glaciology, 14, 1-7(2000-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2907&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766171924284571648 |