@article{oai:kumadai.repo.nii.ac.jp:00021264,
 author = {田中, 健路 and 蒲原, さやか and Kamohara, Sayaka and 山田, 文彦 and 大本, 照憲 and 杉尾, 哲 and Sugio, Satoru and 田中, 健路 and Tanaka, Kenji and 蒲原, さやか and Kamohara, Sayaka and 山田, 文彦 and Yamada, Fumihiko and 大本, 照憲 and Ohmoto, Terunori and 杉尾, 哲 and Sugio, Satoru},
 issue = {4},
 journal = {Natural Hazards Review},
 month = {Nov},
 note = {application/pdf, 論文(Article), Numerical experiments using a mesoscale meteorological model (MM5) are performed to evaluate the mountainous orographical effects on the heavy rainfalls brought by Typhoon 0514 (NABI), which caused the flood disaster in the southeast Kyushu area of Japan.  The terrain conditions considered in the numerical model are three folds: first, a flat terrain with the altitude 1m above mean sea level; second, an idealized line-shaped mountain terrain; third, a complex terrain using GTOPO30.  Although an accumulated rainfall due to Typhoon 0514 is recorded higher than 1,000 mm, a calculated one using the flat terrain is 250-300 mm.  The calculated rainfall using the complex terrain becomes 200-300% (500-900 mm) in comparison to flat terrain case.  This discrepancy is found to cause by blocking and evolving the convective cells, which are generated by lifting up the water vapor along the mountain slope in the windward areas.  A ratio of the forecasted rainfall with/without orography provided an important index for the risk of the heavy rain in the tropical cyclone.},
 pages = {190--198},
 title = {Orographical Effects of Heavy Rainfall by Typhoon 0514 (NABI)},
 volume = {9},
 year = {2008},
 yomi = {カモハラ, サヤカ and スギオ, サトル and タナカ, ケンジ and カモハラ, サヤカ and ヤマダ, フミヒコ and オオモト, テルノリ and スギオ, サトル}
}