Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)

The weather conditions from September to January in the vicinity of the Mizuho Plateau, the area between the coast and 72°S, are discussed on the basis of the weather observations made during the traverses of JARE-10 (the 10th Japanese Antarctic Research Expedition) in 1969-70 and the previous trave...

Full description

Bibliographic Details
Main Author: Yutaka AGETA
Format: Article
Language:English
Published: National Institute of Polar Research 1971-07-01
Series:Antarctic Record
Online Access:https://doi.org/10.15094/00007628
id doaj-4f4a4b8485b14e298f52ee6687d7d5ab
record_format Article
spelling doaj-4f4a4b8485b14e298f52ee6687d7d5ab2020-11-24T23:05:58ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1971-07-0141426110.15094/00007628Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)Yutaka AGETA0Water Research Laboratory, Faculty of Science, Nagoya University The weather conditions from September to January in the vicinity of the Mizuho Plateau, the area between the coast and 72°S, are discussed on the basis of the weather observations made during the traverses of JARE-10 (the 10th Japanese Antarctic Research Expedition) in 1969-70 and the previous traverses. The mean wind speed of about 8-10 m/s is obtained from the observations. It is found that the observed orientations of sastrugis and pitted patterns show seasonal variations. The wind direction is constant in inland, but diurnal variations of the wind direction were observed. When the wind direction changes counterclockwise to the north from the prevailing wind direction, it can be expected that weather is getting worse. The flow lines of the prevailing winds in the vicinity of the Mizuho Plateau are drawn from the orientations of sastrugis and other features. The pressure variation in inland about 350 km distant from Syowa Station was similar to that at Syowa Station. Sea-salt particles were detected at 71°S and 43°E during a light snow or ice prisms falling when the wind was weak with its direction changing counterclockwise from the prevailing wind direction.https://doi.org/10.15094/00007628
collection DOAJ
language English
format Article
sources DOAJ
author Yutaka AGETA
spellingShingle Yutaka AGETA
Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)
Antarctic Record
author_facet Yutaka AGETA
author_sort Yutaka AGETA
title Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)
title_short Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)
title_full Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)
title_fullStr Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)
title_full_unstemmed Some Aspects of the Weather Conditions in the Vicinity of the Mizuho Plateau, East Antarctica (Reports of the Japanese Antarctic Research Expedition)
title_sort some aspects of the weather conditions in the vicinity of the mizuho plateau, east antarctica (reports of the japanese antarctic research expedition)
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 1971-07-01
description The weather conditions from September to January in the vicinity of the Mizuho Plateau, the area between the coast and 72°S, are discussed on the basis of the weather observations made during the traverses of JARE-10 (the 10th Japanese Antarctic Research Expedition) in 1969-70 and the previous traverses. The mean wind speed of about 8-10 m/s is obtained from the observations. It is found that the observed orientations of sastrugis and pitted patterns show seasonal variations. The wind direction is constant in inland, but diurnal variations of the wind direction were observed. When the wind direction changes counterclockwise to the north from the prevailing wind direction, it can be expected that weather is getting worse. The flow lines of the prevailing winds in the vicinity of the Mizuho Plateau are drawn from the orientations of sastrugis and other features. The pressure variation in inland about 350 km distant from Syowa Station was similar to that at Syowa Station. Sea-salt particles were detected at 71°S and 43°E during a light snow or ice prisms falling when the wind was weak with its direction changing counterclockwise from the prevailing wind direction.
url https://doi.org/10.15094/00007628
work_keys_str_mv AT yutakaageta someaspectsoftheweatherconditionsinthevicinityofthemizuhoplateaueastantarcticareportsofthejapaneseantarcticresearchexpedition
_version_ 1725624627924828160