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Dynamical Behaviour of the Ice Sheet on Mizuho Plateau, East Antarctica

Published online by Cambridge University Press:  20 January 2017

Fumihiko Nishio
Affiliation:
National Institute of Polar Research, Kaga 1-9-10, Itabashi-ku, Tokyo 173, Japan
Shinji Mae
Affiliation:
Department of Applied Physics, Faculty of Engineering, Hokkaido University, Sapporo 060, Japan
Hirokazu Ohmae
Affiliation:
Institute of Low Temperature Science, Hokkaido University, Kita-19, Nishi-8, Kita-ku, Sapporo 060, Japan
Masayoshi Nakawo
Affiliation:
Nagaoka Institute of Snow and Ice Studies, National Research Center for Disaster Prevention, Science and Technology Agency, Suyoshi, Nagaoka, Niigata 940, Japan
Shuhei Takahashi
Affiliation:
Κitami Institute of Technology, Κitami 090, Japan
Κunio Kawata
Affiliation:
Faculty of Science, Toyama University, Toyama 930, Japan
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Abstract

Type
Abstracts of Papers Presented at the Symposium but not Published in this Volume
Copyright
Copyright © International Glaciological Society 1989

The Japanese Antarctic Research Expedition (JARE) has continued glaciological work in the Mizuho Plateau, East Antarctica. We have already reported that the ice sheet in Mizuho Plateau, which flows into Shirase Glacier and is classified as a fast-moving outlet glacier was thinning at a rate of about 70 cm/year, and the profile of the basal shear stress along the central flow line was similar to that of surging glaciers.

A new 5 year glaciological programme in Mizuho Plateau and East Dronning Maud Land which started in 1981 is now being carried out, and we have obtained new results as follows:

  1. The ice sheet in the down-stream region where the ice elevation is lower than about 2400 m is thinning, based upon data for horizontal and vertical flow velocity, strain-rate, slope of the ice surface, accumulation rate, and densification of the snow.

  2. δ18O analysis of deep ice cores obtained at Mizuho Station (elevation of 2240 m) and point G2 (elevation of 1730 m) shows that δ18O increased about 2000 years ago at Mizuho Station and about 400 years ago at point G2. If we can assume that the increase in δ18O is caused by the ice-sheet thinning, this result means that the ice-sheet thinning propagates to an up-stream area.

  3. The result of radio echo-sounding on Mizuho Plateau suggests that the base of the ice sheet in the down-stream region is wet. Based upon three-dimensional numerical modelling, the calculated bottom temperature shows that the ice temperature at the base of the ice sheet in the glacier down-stream is higher than the melting point and that the ice base is also wet. These results support the result described in (1), since the basal sliding due to a wet base causes ice-sheet thinning as suggested by our previous studies.

Summarizing these results, a possible explanation of ice-sheet variation on Mizuho Plateau is as follows: the thinning of the ice sheet caused by the basal sliding due to melting of the ice base began at Shirase Glacier and has been expanding to an up-stream area to reach the present state. A simple calculation, using flow velocities, shows that the thinning began at Shirase Glacier about 1500–2000 years ago.

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