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Typhoon and ENSO simulation using a high-resolution coupled GCM
https://nied-repo.bosai.go.jp/records/4448
https://nied-repo.bosai.go.jp/records/4448a45fc71e-1ef6-4a14-9c11-acbc312a00da
| Item type | researchmap(1) | |||||||||||||
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| 公開日 | 2023-03-30 | |||||||||||||
| タイトル | ||||||||||||||
| 言語 | en | |||||||||||||
| タイトル | Typhoon and ENSO simulation using a high-resolution coupled GCM | |||||||||||||
| 言語 | ||||||||||||||
| 言語 | eng | |||||||||||||
| 著者 |
Tomonori Matsuura
× Tomonori Matsuura
× Michiaki Yumoto
× Satoshi Iizuka
× Ryuichi Kawamura
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| 抄録 | ||||||||||||||
| 内容記述タイプ | Other | |||||||||||||
| 内容記述 | The relationship between the character of tropical storm (TS) activity in the northwestern equatorial Pacific (NWEP) and the El Nino-Southern Oscillation (ENSO) is investigated from the viewpoint of how TS behavior varies interannually. A high-resolution coupled general circulation model (CGCM) capable of simultaneously reproducing both TSs and ENSOs has been developed to study the role of air-sea interaction in linking TS activity with ENSO. Analysis of 15 years simulation and observations shows that TS frequency decreases slightly off the Philippine Islands (120 degrees E-150 degrees E, 5 degrees N-20 degrees N) and that the location of their generation shifts toward the east during El Nino years. This results in inactive convection in the NWEP during El Nino years due to an increase in sea level pressure over ocean areas. | |||||||||||||
| 言語 | en | |||||||||||||
| 書誌情報 |
en : GEOPHYSICAL RESEARCH LETTERS 巻 26, 号 12, p. 1755-1758 |
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| 出版者 | ||||||||||||||
| 言語 | en | |||||||||||||
| 出版者 | AMER GEOPHYSICAL UNION | |||||||||||||
| ISSN | ||||||||||||||
| 収録物識別子タイプ | ISSN | |||||||||||||
| 収録物識別子 | 0094-8276 | |||||||||||||
| DOI | ||||||||||||||
| 関連識別子 | 10.1029/1999GL900329 | |||||||||||||
