@article{oai:rakuno.repo.nii.ac.jp:00007011,
 author = {馬場, 賢治 and 猪又, 淳之助},
 issue = {2},
 journal = {酪農学園大学紀要. 自然科学編},
 month = {Mar},
 note = {Bulletin, The outer rainbands of Typhoon 1611 (LIONROCK), which caused heavy rainfall in the Tokachi region of Hokkaido from August 29 to 31, 2016, were analyzed by the Nagoya University Cloud-Resolving Storm Simulator (CReSS) at a 2 km grid size. From the meteorological radar observations of the Japan meteorological agency, rainbands were distributed from the Tokachi area in the east-southeast and east-southeast directions, respectively, were successfully simulated using CReSS. The rainband advected from the south-southeast had an equivalent potential temperature exceeding 340 K, indicator heavy rainfall, and in the northern region, a shear line of winds in the southeast and south-southeast was formed having unstable atmospheric conditions. Results show this disturbance directed to the Hidaka and Ishikari mountains, increased precipitation due to the influence of mountain slopes.},
 pages = {81--90},
 title = {2016年台風10号接近に伴う日高山脈と石狩山地における降水帯構造},
 volume = {46},
 year = {2022}
}