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dc.contributor.author | 吉岡, 大秋 | ja |
dc.contributor.author | 榎本, 剛 | ja |
dc.contributor.alternative | YOSHIOKA, Hiroaki | en |
dc.contributor.alternative | ENOMOTO, Takeshi | en |
dc.contributor.transcription | ヨシオカ, ヒロアキ | ja-Kana |
dc.contributor.transcription | エノモト, タケシ | ja-Kana |
dc.date.accessioned | 2018-12-25T23:39:23Z | - |
dc.date.available | 2018-12-25T23:39:23Z | - |
dc.date.issued | 2018-09 | - |
dc.identifier.issn | 0386-412X | - |
dc.identifier.uri | http://hdl.handle.net/2433/235858 | - |
dc.description.abstract | The influence of the Coriolis force influence on the intensity of Hurricane PALI that was generated at 4.4°N on 18Z 7 January 2016 was examined. Ensemble downscale experiments were conducted using the nonhydrostatic meso-scale numerical model, the Weather Research and Forecasting Model (WRF), with horizontal resolution of 10 km from the initial states derived from 11 ensemble members of NOAA's 2nd-generation global ensemble reforecast dataset. Sensitivity to the intensity is identified by initial time from 00Z 1 January to 00Z 10 every 24 hours. All disturbances with different develop to the intensity of Tropical cyclone (17.0 ms-1). By changing initial time, the score of root mean square error of maximum wind speed has changed and 00Z 3 (about 5days before PALI genesis) is including the best score member. In the best member experiment, an analysis was carried out by selecting the stagnation period and the development period. Super-gradient wind, which means that tangential wind speed is larger than gradient wind speed, during the development period is larger than during the stagnation period. | en |
dc.format.mimetype | application/pdf | - |
dc.language.iso | jpn | - |
dc.publisher | 京都大学防災研究所 | ja |
dc.publisher.alternative | Disaster Prevention Research Institute, Kyoto University | en |
dc.subject | 熱帯低気圧 | ja |
dc.subject | ハリケーン | ja |
dc.subject | 強度 | ja |
dc.subject | 傾度風平衡 | ja |
dc.subject | Tropical Cyclone | en |
dc.subject | Hurricane | en |
dc.subject | Intensity | en |
dc.subject | Gradient Wind Balance | en |
dc.subject.ndc | 519.9 | - |
dc.title | 低緯度におけるハリケーン強化過程のダウンスケール実験 | ja |
dc.title.alternative | Downscale Experiments of the Hurricane Intensification at Low Latitudes | en |
dc.type | departmental bulletin paper | - |
dc.type.niitype | Departmental Bulletin Paper | - |
dc.identifier.ncid | AN00027784 | - |
dc.identifier.jtitle | 京都大学防災研究所年報. B | ja |
dc.identifier.volume | 61 | - |
dc.identifier.issue | B | - |
dc.identifier.spage | 380 | - |
dc.identifier.epage | 386 | - |
dc.textversion | publisher | - |
dc.sortkey | 19 | - |
dc.address | 京都大学大学院理学研究科 | ja |
dc.address | 京都大学防災研究所 | ja |
dc.address.alternative | Graduate School of Science, Kyoto University | en |
dc.address.alternative | Disaster Prevention Research Institute Kyoto University | en |
dc.relation.url | http://www.dpri.kyoto-u.ac.jp/publications/nenpo/ | - |
dcterms.accessRights | open access | - |
datacite.awardNumber | JP26282111 | - |
dc.identifier.pissn | 0386-412X | - |
dc.identifier.jtitle-alternative | Disaster Prevention Research Institute Annuals. B | en |
jpcoar.funderName | 日本学術振興会 | ja |
jpcoar.funderName.alternative | Japan Society for the Promotion of Science (JSPS) | en |
出現コレクション: | Vol.61 B |
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