@article{oai:tokyo-metro-u.repo.nii.ac.jp:00002885,
 author = {ヤマカワ, シュウジ and Yamakawa, Shuji},
 issue = {26},
 journal = {Geographical Reports of Tokyo Metropolitan University},
 month = {},
 note = {A weather system before and after a cold front passage over North Japan is studied from the viewpoint of mesoscale and synoptic scale meteorology. A case study in winter shows the typical synoptic system and distinctive mesoscale phenomena. The temporal and regional features of temperature variations, which are accompanied by the pass of a cold front, are focused on. For example, in Nemuro Plain, the inland of southeastern Hokkaido, temperature rises suddenly and temporarily right after the cold front passage, chiefly because the inversion layers are destroyed by downslope wind on the lee side. This exceptional weather system is worth noting not only in meteorology but also in synoptic climatology.},
 pages = {11--21},
 title = {Weather systems of winter passing cold front over north japan},
 year = {1991}
}