@article{oai:ous.repo.nii.ac.jp:00001096,
 author = {大亀, 衛 and Ohkame, Mamoru and 森脇, 三幸 and Moriwaki, Mituyuki},
 journal = {岡山理科大学紀要. A, 自然科学, Bulletin of Okayama University of Science. A, Natural Sciences},
 month = {Mar},
 note = {P(論文), 角をまわる流れに対応する複素速度ポテンシャルを用いると, 那岐山周辺の風速と流線が数値計算して求められる。更に, ベルヌーイの式を用いると, 気圧が求められる。山裾の風速が大きくなると, 強風が那岐山頂附近に現われる。この風速は山裾の風速に比例しており, 山頂附近の風速は山裾に居て測定される。, The velocity of the wind and stream lines around Mt. Nagi are culculated with complex velocity potential corresponding to the wind stream around the mountain corner. Pressure is figured by using Bernoulli's theorem. If the velocity of the wind increases at the foot of the mountain, strong wind rises above the top of the mountain. Its velocity increases in proportion to that at the foot of the mountain. Thus, the strong wind above the top of the mountain is estimated based on the wind velocity at the foot of the mountain.},
 pages = {75--82},
 title = {那岐山頂附近の風(広戸風)},
 volume = {30},
 year = {1995},
 yomi = {オオカメ, マモル and モリワキ, ミツユキ}
}