Oxygen Isotope Profiles in Firn Cores from Mizuho Plateau, Antarctica

Oxygen isotope, gross β-radioactivity and stratigraphic determinations were done on firn cores from Mizuho Plateau, Antarctica. Factors controlling oxygen isotope variations in firn were discussed. From the results of gross β-activity measurements, it is obvious that the cycle in oxygen isotope prof...

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Bibliographic Details
Main Authors: Kikuo KATO, Okitsugu WATANABE
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1977
Subjects:
Online Access:https://doi.org/10.15094/00007924
https://doaj.org/article/5c003b66720f409fa4acc38d376c9d04
Description
Summary:Oxygen isotope, gross β-radioactivity and stratigraphic determinations were done on firn cores from Mizuho Plateau, Antarctica. Factors controlling oxygen isotope variations in firn were discussed. From the results of gross β-activity measurements, it is obvious that the cycle in oxygen isotope profile is once a year in some areas due to the seasonal variation in oxygen isotopic composition of snowfall. In other areas, the cycle is not once a year. The following two factors are considered to affect strongly oxygen isotope variations in firn, from the results of direct stake measurements of snow accumulation and observations of surface conditions of the ice sheet. 1) changes in time of erosion, deposition and none on snow surface, 2) subsequent movement of water vapor in firn.