@article{oai:tokyo-metro-u.repo.nii.ac.jp:00002952,
 author = {タナカ, ヒロハル and タニモト, ヨウイチ and ミカミ, タケヒコ and Tanaka, Hiroharu and Tanimoto, Youichi and Mikami, Takehiko},
 issue = {33},
 journal = {Geographical Reports of Tokyo Metropolitan University},
 month = {},
 note = {We examined a thermal structure on the mountain slope over clean calm nights at the southern Mt. Yatsugatake, central Japan. Meteorological observations showed double thermal inversions over the slope. The upper one appeared between approximately 1800 m and 2000 m a.s.l. (1100 m and 1300 m from surface), and the lower one, between 700 m and 950 m a.s.l. (surface and 250 m from surface). Successive snapshots of a thermography showed horizontal bands of this upper inversion clearly. Radiosonde data in this field indicated that this thermal structure on the slope was associated with the thermo-dynamical processes in the atmospheric boundary layer: the upper inversion forced by the adiabatic warming by subsidence but the lower one forced by the radiative surface cooling.},
 pages = {21--31},
 title = {The relationship between double thermal inversions and thermal belt in the mt. yatsugatake area, central japan},
 year = {1998}
}