@article{oai:nipr.repo.nii.ac.jp:00003706,
 author = {タカハシ, シュウヘイ and エンドウ, タツオ and アズマ, ノブヒコ and メシダ, シゲミ and TAKAHASHI, Shuhei and ENDOH, Tatsuo and AZUMA, Nobuhiko and MESHIDA, Shigemi},
 journal = {Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology},
 month = {Feb},
 note = {P(論文), Observations of a bare ice field was carried out at Seal Rock in the S∅r Rondane area, East Antarctica. A large sublimation rate, 200 to 280mm/a, was observed on the bare ice field. Air temperature on the bare ice was about 1℃ higher than that on snow surface. The large sublimation rate was explained from the low albedo of bare ice; its value was roughly estimated from heat budget considerations. The bare ice fields were classified into 4 types according to origin.},
 pages = {128--139},
 title = {BARE ICE FIELDS DEVELOPED IN THE INLAND PART OF ANTARCTICA},
 volume = {5},
 year = {1992}
}