Chemical composition of snow drift on Mizuho Plateau
P(論文) The chemical composition was determined on snow drift which was sampled at Mizuho Station (2230m a. s. l.) and Mizuho Plateau (1800-3000m a. s. l.), East Antarctica, in 1986. Na^+, Cl^-, NO_3^- and SO_4^<2-> were determined by ion chromatography on 44 samples. Electroconductivity and H^+...
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Language: | English |
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National Institute of Polar Research
1989
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Online Access: | https://nipr.repo.nii.ac.jp/record/3566/files/KJ00000035532.pdf https://doi.org/10.15094/00003566 https://nipr.repo.nii.ac.jp/records/3566 |
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author | Osada, Kazuo Ohmae, Hirokazu Nishio, Fumihiko Higuchi, Keiji Kanamori, Satoru |
author_facet | Osada, Kazuo Ohmae, Hirokazu Nishio, Fumihiko Higuchi, Keiji Kanamori, Satoru |
author_sort | Osada, Kazuo |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) The chemical composition was determined on snow drift which was sampled at Mizuho Station (2230m a. s. l.) and Mizuho Plateau (1800-3000m a. s. l.), East Antarctica, in 1986. Na^+, Cl^-, NO_3^- and SO_4^<2-> were determined by ion chromatography on 44 samples. Electroconductivity and H^+ concentration were also measured on 85 samples. The concentrations of NO_3^- and SO_4^<2-> of snow drift showed maximum values in summer. It is considered that the concentrations of both Na^+ and Cl^- of snow drift during winter are dependent on not only the amount of sea-salt in the atmosphere but also on the dilution effect through mixing with falling snow. It is pointed out that increase in their concentrations of snow drift in late summer results from aerosol scavenged by drifting snow particles rather than sublimation of drifting snow particles. departmental bulletin paper |
genre | Antarc* Antarctica East Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
genre_facet | Antarc* Antarctica East Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
geographic | East Antarctica Mizuho Mizuho Station Mizuho Plateau |
geographic_facet | East Antarctica Mizuho Mizuho Station Mizuho Plateau |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00003566 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(44.317,44.317,-70.683,-70.683) ENVELOPE(44.317,44.317,-70.683,-70.683) ENVELOPE(40.000,40.000,-73.000,-73.000) |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00003566 |
op_relation | Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 2 70 78 AA10756213 https://nipr.repo.nii.ac.jp/record/3566/files/KJ00000035532.pdf https://doi.org/10.15094/00003566 https://nipr.repo.nii.ac.jp/records/3566 |
publishDate | 1989 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00003566 2025-04-13T14:09:43+00:00 Chemical composition of snow drift on Mizuho Plateau Osada, Kazuo Ohmae, Hirokazu Nishio, Fumihiko Higuchi, Keiji Kanamori, Satoru 1989-08 application/pdf https://nipr.repo.nii.ac.jp/record/3566/files/KJ00000035532.pdf https://doi.org/10.15094/00003566 https://nipr.repo.nii.ac.jp/records/3566 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 2 70 78 AA10756213 https://nipr.repo.nii.ac.jp/record/3566/files/KJ00000035532.pdf https://doi.org/10.15094/00003566 https://nipr.repo.nii.ac.jp/records/3566 1989 ftnipr https://doi.org/10.15094/00003566 2025-03-19T10:19:56Z P(論文) The chemical composition was determined on snow drift which was sampled at Mizuho Station (2230m a. s. l.) and Mizuho Plateau (1800-3000m a. s. l.), East Antarctica, in 1986. Na^+, Cl^-, NO_3^- and SO_4^<2-> were determined by ion chromatography on 44 samples. Electroconductivity and H^+ concentration were also measured on 85 samples. The concentrations of NO_3^- and SO_4^<2-> of snow drift showed maximum values in summer. It is considered that the concentrations of both Na^+ and Cl^- of snow drift during winter are dependent on not only the amount of sea-salt in the atmosphere but also on the dilution effect through mixing with falling snow. It is pointed out that increase in their concentrations of snow drift in late summer results from aerosol scavenged by drifting snow particles rather than sublimation of drifting snow particles. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Plateau ENVELOPE(40.000,40.000,-73.000,-73.000) |
spellingShingle | Osada, Kazuo Ohmae, Hirokazu Nishio, Fumihiko Higuchi, Keiji Kanamori, Satoru Chemical composition of snow drift on Mizuho Plateau |
title | Chemical composition of snow drift on Mizuho Plateau |
title_full | Chemical composition of snow drift on Mizuho Plateau |
title_fullStr | Chemical composition of snow drift on Mizuho Plateau |
title_full_unstemmed | Chemical composition of snow drift on Mizuho Plateau |
title_short | Chemical composition of snow drift on Mizuho Plateau |
title_sort | chemical composition of snow drift on mizuho plateau |
url | https://nipr.repo.nii.ac.jp/record/3566/files/KJ00000035532.pdf https://doi.org/10.15094/00003566 https://nipr.repo.nii.ac.jp/records/3566 |