@article{oai:nipr.repo.nii.ac.jp:00008957,
 author = {金戸, 進 and Kaneto, Susumu},
 issue = {1},
 journal = {南極資料, Antarctic Record},
 month = {Mar},
 note = {P(論文), 南極域における気候変動に関する総合研究(ACR)期間中(1987年-1991年)の昭和基地とあすか観測拠点の気象経過を, 過去の気象データと比較するなどして, その特徴を示した。昭和基地では期間前半, 風が弱く周辺の海氷上では積雪の少ない状態が続き夏期間に海氷の流出がたびたびあった。下部成層圏では1988年春に過去最大級の突然昇温を観測したが, 極渦の解消には至らなかったとみられる。あすか観測拠点では, ほぼ5年間のデータが得られ, 内陸基地では最も大きい年平均風速12.6m/sを記録した。, Meteorological data obtained at Syowa Station and Asuka Station during the Antarctic Climate Research (ACR) period (1987-1991) are analyzed compared with normal values and Mizuho Station data. At Syowa, the first half of the period was characterized by weak wind and less snow accumulation, and sea ice around Syowa blew offshore during the summer season frequently. In the lower stratosphere, the largest sudden warming was observed over Syowa in the spring of 1988,but the polar vortex did not decay as one would expect. At Asuka, 5 years of data were obtained. It was revealed that the yearly mean wind speed is largest at inland stations.},
 pages = {1--8},
 title = {昭和基地周辺の気象経過},
 volume = {41},
 year = {1997},
 yomi = {カネト, ススム}
}