The enso-asian monsoon interaction in a coupled ocean-atmosphere gcm
文献类型：期刊论文
| 作者 | Li, Ying; Lu, Riyu; Dong, Buwen |
| 刊名 | Journal of climate
 |
| 出版日期 | 2007-10-15 |
| 卷号 | 20期号:20页码:5164-5177 |
| ISSN号 | 0894-8755 |
| DOI | 10.1175/jcli4289.1 |
| 通讯作者 | Li, ying() |
| 英文摘要 | In this study, the authors evaluate the ( el nino-southern oscillation) enso-asian monsoon interaction in a version of the hadley centre coupled ocean-atmosphere general circulation model ( cgcm) known as hadcm3. the main focus is on two evolving anomalous anticyclones: one located over the south indian ocean ( sio) and the other over the western north pacific ( wnp). these two anomalous anticyclones are closely related to the developing and decaying phases of the enso and play a crucial role in linking the asian monsoon to enso. it is found that the hadcm3 can well simulate the main features of the evolution of both anomalous anticyclones and the related sst dipoles, in association with the different phases of the enso cycle. by using the simulated results, the authors examine the relationship between the wnp/sio anomalous anticyclones and the enso cycle, in particular the biennial component of the relationship. it is found that a strong el nino event tends to be followed by a more rapid decay and is much more likely to become a la nina event in the subsequent winter. the twin anomalous anticyclones in the western pacific in the summer of a decaying el nino are crucial for the transition from an el nino into a la nina. the el nino ( la nina) events, especially the strong ones, strengthen significantly the correspondence between the sio anticyclonic ( cyclonic) anomaly in the preceding autumn and wnp anticyclonic ( cyclonic) anomaly in the subsequent spring, and favor the persistence of the wnp anomaly from spring to summer. the present results suggest that both el nino ( la nina) and the sio/wnp anticyclonic ( cyclonic) anomalies are closely tied with the tropospheric biennial oscillation ( tbo). in addition, variability in the east asian summer monsoon, which is dominated by the internal atmospheric variability, seems to be responsible for the appearance of the wnp anticyclonic anomaly through an upper-tropospheric meridional teleconnection pattern over the western and central pacific. |
| WOS关键词 | WESTERN NORTH PACIFIC ; NINO SOUTHERN-OSCILLATION ; EL-NINO ; SUMMER MONSOON ; TROPICAL PACIFIC ; INDIAN-OCEAN ; INTERCOMPARISON PROJECT ; INTERANNUAL VARIABILITY ; BIENNIAL OSCILLATION ; FLUX ADJUSTMENTS |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| WOS类目 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000250105900010 |
| 出版者 | AMER METEOROLOGICAL SOC |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2380055 |
| 专题 | 中国科学院大学 |
| 通讯作者 | Li, Ying |
| 作者单位 | 1.Chinese Acad Sci, Inst Atmospher Phys, CMSR, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Inst Atmospher Phys, LASG, Beijing, Peoples R China 4.Univ Reading, Walker Inst Climate Syst Res, Reading, Berks, England 5.Natl Ctr Atmospher Sci Climate, Reading, Berks, England |
| 推荐引用方式 GB/T 7714 | Li, Ying,Lu, Riyu,Dong, Buwen. The enso-asian monsoon interaction in a coupled ocean-atmosphere gcm[J]. Journal of climate,2007,20(20):5164-5177. |
| APA | Li, Ying,Lu, Riyu,&Dong, Buwen.(2007).The enso-asian monsoon interaction in a coupled ocean-atmosphere gcm.Journal of climate,20(20),5164-5177. |
| MLA | Li, Ying,et al."The enso-asian monsoon interaction in a coupled ocean-atmosphere gcm".Journal of climate 20.20(2007):5164-5177. |
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来源：中国科学院大学
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