The Bedrock Topography Deduced from Multiple Radar Echoes Observed in the Mizuho Plateau, East Antarctica

Taking into account the effect of spatial fading and erronous echoes caused by large scale undulations of bedrock surface, the radar echo data by the 14th Japanese Antarctic Research Expedition were reanalysed to obtain the ice thickness and bedrock topography in the Mizuho Plateau area. The bedrock...

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Bibliographic Details
Main Author: Shinji MAE
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1978
Subjects:
Online Access:https://doi.org/10.15094/00007980
https://doaj.org/article/212d5493810a4ab0805970d11cd966a7
Description
Summary:Taking into account the effect of spatial fading and erronous echoes caused by large scale undulations of bedrock surface, the radar echo data by the 14th Japanese Antarctic Research Expedition were reanalysed to obtain the ice thickness and bedrock topography in the Mizuho Plateau area. The bedrock topographies along three Routes A, C and S are drawn by solid lines in Figs. 3, 4 and 5 respectively. Even though slopes on the bedrock were smoothened, there remain some steep ones which satisfy the condition of the existence of a sub-ice water lake. Since it was expected from the data of surface velocity measurements along Route A that the basal sliding was taking placing with the ice sheet north of Route A in the Mizuho Plateau, it is probable that there exist a sub-ice water lake along the valley indicated by a dotted line V-W in Fig. 2.