Formation of Surface Snow Layer at Mizuho Station, Antarctica

P(論文) On the basis of year round observations of surface snow condition in 1977 and snow stake measurements carried out from 1972 to 1978 at Mizuho Station, which is located at 70°42′S, 44°20′E and 2230m a. s. l. in the katabatic wind region, daily, seasonal and secular changes of surface condition...

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Main Author: Fujii, Yoshiyuki
Language:English
Published: 1981
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1189/files/KJ00000011715.pdf
https://nipr.repo.nii.ac.jp/records/1189
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author Fujii, Yoshiyuki
author_facet Fujii, Yoshiyuki
author_sort Fujii, Yoshiyuki
collection National Institute of Polar Research Repository, Japan
description P(論文) On the basis of year round observations of surface snow condition in 1977 and snow stake measurements carried out from 1972 to 1978 at Mizuho Station, which is located at 70°42′S, 44°20′E and 2230m a. s. l. in the katabatic wind region, daily, seasonal and secular changes of surface condition and surface layer formation are studied. The surface level changes gradually by sublimation in summer and condensation in winter, and rapidly by deposition and wind erosion of snow. Surface features change much in the intermediate seasons, when low pressure disturbances is active, between summer and winter. The alternative years variation is seen in the mean annual balance of 202 stakes in 1973-1977,being high in 1973,1975 and 1977 and low in 1974 and 1976. Formation of an annual layer occurs once in two or three years on the average. The mean, maximum and minimum annual balance of 202 stakes in 1973-1977 are 1.5-14.8cm, 36.0-52.1cm and -10.4∿-14.9cm, respectively. The absence of annual layer or layers is mainly due to no deposition of snow and to sublimation of a pre-formed annual layer or layers. A model of transmigration of the surface condition is proposed. departmental bulletin paper
genre Antarc*
Antarctica
Memoirs of National Institute of Polar Research
Polar Research
genre_facet Antarc*
Antarctica
Memoirs of National Institute of Polar Research
Polar Research
geographic Mizuho
Mizuho Station
geographic_facet Mizuho
Mizuho Station
id ftnipr:oai:nipr.repo.nii.ac.jp:00001189
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)
op_collection_id ftnipr
op_relation Memoirs of National Institute of Polar Research. Special issue
19
280
296
AA00733561
https://nipr.repo.nii.ac.jp/record/1189/files/KJ00000011715.pdf
https://nipr.repo.nii.ac.jp/records/1189
publishDate 1981
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001189 2025-04-13T14:10:16+00:00 Formation of Surface Snow Layer at Mizuho Station, Antarctica Fujii, Yoshiyuki 1981-10 application/pdf https://nipr.repo.nii.ac.jp/record/1189/files/KJ00000011715.pdf https://nipr.repo.nii.ac.jp/records/1189 eng eng Memoirs of National Institute of Polar Research. Special issue 19 280 296 AA00733561 https://nipr.repo.nii.ac.jp/record/1189/files/KJ00000011715.pdf https://nipr.repo.nii.ac.jp/records/1189 1981 ftnipr 2025-03-19T10:19:56Z P(論文) On the basis of year round observations of surface snow condition in 1977 and snow stake measurements carried out from 1972 to 1978 at Mizuho Station, which is located at 70°42′S, 44°20′E and 2230m a. s. l. in the katabatic wind region, daily, seasonal and secular changes of surface condition and surface layer formation are studied. The surface level changes gradually by sublimation in summer and condensation in winter, and rapidly by deposition and wind erosion of snow. Surface features change much in the intermediate seasons, when low pressure disturbances is active, between summer and winter. The alternative years variation is seen in the mean annual balance of 202 stakes in 1973-1977,being high in 1973,1975 and 1977 and low in 1974 and 1976. Formation of an annual layer occurs once in two or three years on the average. The mean, maximum and minimum annual balance of 202 stakes in 1973-1977 are 1.5-14.8cm, 36.0-52.1cm and -10.4∿-14.9cm, respectively. The absence of annual layer or layers is mainly due to no deposition of snow and to sublimation of a pre-formed annual layer or layers. A model of transmigration of the surface condition is proposed. departmental bulletin paper Other/Unknown Material Antarc* Antarctica Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683)
spellingShingle Fujii, Yoshiyuki
Formation of Surface Snow Layer at Mizuho Station, Antarctica
title Formation of Surface Snow Layer at Mizuho Station, Antarctica
title_full Formation of Surface Snow Layer at Mizuho Station, Antarctica
title_fullStr Formation of Surface Snow Layer at Mizuho Station, Antarctica
title_full_unstemmed Formation of Surface Snow Layer at Mizuho Station, Antarctica
title_short Formation of Surface Snow Layer at Mizuho Station, Antarctica
title_sort formation of surface snow layer at mizuho station, antarctica
url https://nipr.repo.nii.ac.jp/record/1189/files/KJ00000011715.pdf
https://nipr.repo.nii.ac.jp/records/1189