Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975

Measurements were carried out simultaneously of drifting snow and wind speed over the surface from 1974 to 1975 at Mizuho Camp using an improved drawer-type drift collector which had a collection efficiency of about 0.55. From the obtained profile of spatial distribution of drift mass flux, it is co...

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Main Authors: Masayuki Inoue, Kazuo Fujino
Format: Article
Language:English
Published: National Institute of Polar Research 1977-11-01
Series:Antarctic Record
Online Access:https://doi.org/10.15094/00007960
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author Masayuki Inoue
Kazuo Fujino
author_facet Masayuki Inoue
Kazuo Fujino
author_sort Masayuki Inoue
collection DOAJ
description Measurements were carried out simultaneously of drifting snow and wind speed over the surface from 1974 to 1975 at Mizuho Camp using an improved drawer-type drift collector which had a collection efficiency of about 0.55. From the obtained profile of spatial distribution of drift mass flux, it is considered that a layer from the surface to a height of about 25 cm is the one in which the saltation of snow particles prevails and a layer on top of it is the one in which snow particles are suspended by turbulent diffusion. A significant correlation was found between the total drift transport and the wind speed at the height of 10 m above the surface. The total drift transport at Mizuho Camp evaluated from this correlation was about 0.64×10^6 ton・km^<-1>・year^<-1>.
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spelling doaj.art-bcf33f7cc17649dfad8847e7a86b9cc92022-12-22T00:12:09ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1977-11-016011210.15094/00007960Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975Masayuki Inoue0Kazuo Fujino1The Institute of Low Temperature Science, Hokkaido UniversityThe Institute of Low Temperature Science, Hokkaido University Measurements were carried out simultaneously of drifting snow and wind speed over the surface from 1974 to 1975 at Mizuho Camp using an improved drawer-type drift collector which had a collection efficiency of about 0.55. From the obtained profile of spatial distribution of drift mass flux, it is considered that a layer from the surface to a height of about 25 cm is the one in which the saltation of snow particles prevails and a layer on top of it is the one in which snow particles are suspended by turbulent diffusion. A significant correlation was found between the total drift transport and the wind speed at the height of 10 m above the surface. The total drift transport at Mizuho Camp evaluated from this correlation was about 0.64×10^6 ton・km^<-1>・year^<-1>.https://doi.org/10.15094/00007960
spellingShingle Masayuki Inoue
Kazuo Fujino
Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975
Antarctic Record
title Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975
title_full Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975
title_fullStr Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975
title_full_unstemmed Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975
title_short Measurements at drifting snow at Mizuho Camp, East Antarctica , 1974-1975
title_sort measurements at drifting snow at mizuho camp east antarctica 1974 1975
url https://doi.org/10.15094/00007960
work_keys_str_mv AT masayukiinoue measurementsatdriftingsnowatmizuhocampeastantarctica19741975
AT kazuofujino measurementsatdriftingsnowatmizuhocampeastantarctica19741975