@article{oai:kitami-it.repo.nii.ac.jp:00007202, author = {Kameda, Takao and Azuma, Nobuhiko and Furukawa, Teruo and Ageta, Yutaka and Takahashi, Shuhei}, journal = {Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology}, month = {2016-11-22}, note = {The paper focuses on the first year-round observations of surface mass balance,sublimation and snow temperatures at Dome Fuji Station. This Station was newly established at the highest point(77°19′0l′′S,39°42′12′′E;381Om)in Queen Maud Land,Antarctica by the Japanese Antarctic Research Expedition. It was found that average surface mass balance by the stake method was +2.5gcm^<-2> from 25 January 1995 to 30 January 1996(370 days),of which about 95% of the positive balance was obtained from February to the middle of October(eight and half months). Sublimation from atmosphere to snow surface (mass input:+0.55gcm^<-2>)was predominant in winter(March to October)and sublimation from snow surface to atmosphere (mass output: -0.39gcm^<-2>) was predominant in summer (November to February).In the annual balance,sublimation from atmosphere to snow surface (+0.16gcm^<-2>) prevailed. This corresponds to about 6% of the annual surface mass balance. The snow temperature at 10 m depth varied from -57.0 to -57.8℃,and the annual mean 10 m snow temperature was -57.3℃., application/pdf}, pages = {24--34}, title = {Surface mass balance, sublimation and snow temperatures at Dome Fuji Station, Antarctica, in 1995}, volume = {11}, year = {} }