@article{oai:niigata-u.repo.nii.ac.jp:00027991,
 author = {堀江, 宏伸 and 小林, 俊一 and 和泉, 薫 and 河島, 克久 and 遠藤, 徹 and 小倉, 康子},
 journal = {新潟大学積雪地域災害研究センター研究年報, 新潟大学積雪地域災害研究センター研究年報},
 month = {Dec},
 note = {We measured the cross-sectional variation of snow depth at four places and investigated stratigraphy of snow wall at one place in Kamakurazawa river, Niigata Prefecture on February 9, 2001. In Kamakurazawa river, the slushflow have frequently occurred. We mainly compared the snow depth in stream side with bank side of the river. We estimate that the average water equivalent of the river channel is about 80% of that outside the river channel. The compacted snow remains in the shade of the bank. The snow pack in the river channel can easily flow if snow becomes wet with the increased runoff and decreases its hardness.},
 pages = {17--26},
 title = {2001年2月9日の新潟県南魚沼郡塩沢町鎌倉沢における河川内積雪水当量および積雪層構造},
 volume = {23},
 year = {2001}
}