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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Main Authors: Osada, Kazuo, Ohmae, Hirokazu, Nishio, Fumihiko, Higuchi, Keiji, Kanamori, Satoru
Language:English
Published: National Institute of Polar Research 1989
Subjects:
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
_version_ 1829301561591857152
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