IMPACTS OF THE TROPICAL PACIFIC COUPLED PROCESS ON THE INTERANNUAL VARIABILITY IN THE INDIAN OCEAN
文献类型:期刊论文
作者 | Feng Jun-qiao1,2; Bai Xue-zhi1,2 |
刊名 | JOURNAL OF TROPICAL METEOROLOGY
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出版日期 | 2010-09-01 |
卷号 | 16期号:3页码:271-279 |
关键词 | Coupled Gcm Iod Tropical Pacific Ocean Enso |
ISSN号 | 1006-8775 |
DOI | 10.3969/j.issn.1006-8775.2010.03.009 |
文献子类 | Article |
英文摘要 | The basic features of climatology and interannual variations of tropical Pacific and Indian Oceans were analyzed using a coupled general circulation model (CGCM), which was constituted with an intermediate 2.5-layer ocean model and atmosphere model ECHAM4. The CGCM well captures the spatial and temporal structure of the Pacific El Nino-Southern Oscillation (ENSO) and the variability features in the tropical Indian Ocean. The influence of Pacific air-sea coupled process on the Indian Ocean variability was investigated carefully by conducting numerical experiments. Results show that the occurrence frequency of positive/negative Indian Ocean Dipole (IOD) event will decrease/increase with the presence/absence of the coupled process in the Pacific Ocean. Further analysis demonstrated that the air-sea coupled process in the Pacific Ocean affects the IOD variability mainly by influencing the zonal gradient of thermocline via modulating the background sea surface wind.; The basic features of climatology and interannual variations of tropical Pacific and Indian Oceans were analyzed using a coupled general circulation model (CGCM), which was constituted with an intermediate 2.5-layer ocean model and atmosphere model ECHAM4. The CGCM well captures the spatial and temporal structure of the Pacific El Nino-Southern Oscillation (ENSO) and the variability features in the tropical Indian Ocean. The influence of Pacific air-sea coupled process on the Indian Ocean variability was investigated carefully by conducting numerical experiments. Results show that the occurrence frequency of positive/negative Indian Ocean Dipole (IOD) event will decrease/increase with the presence/absence of the coupled process in the Pacific Ocean. Further analysis demonstrated that the air-sea coupled process in the Pacific Ocean affects the IOD variability mainly by influencing the zonal gradient of thermocline via modulating the background sea surface wind. |
学科主题 | Meteorology & Atmospheric Sciences |
URL标识 | 查看原文 |
语种 | 英语 |
WOS记录号 | WOS:000282140300009 |
公开日期 | 2010-12-24 |
源URL | [http://ir.qdio.ac.cn/handle/337002/5279] ![]() |
专题 | 海洋研究所_海洋环流与波动重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China |
推荐引用方式 GB/T 7714 | Feng Jun-qiao,Bai Xue-zhi. IMPACTS OF THE TROPICAL PACIFIC COUPLED PROCESS ON THE INTERANNUAL VARIABILITY IN THE INDIAN OCEAN[J]. JOURNAL OF TROPICAL METEOROLOGY,2010,16(3):271-279. |
APA | Feng Jun-qiao,&Bai Xue-zhi.(2010).IMPACTS OF THE TROPICAL PACIFIC COUPLED PROCESS ON THE INTERANNUAL VARIABILITY IN THE INDIAN OCEAN.JOURNAL OF TROPICAL METEOROLOGY,16(3),271-279. |
MLA | Feng Jun-qiao,et al."IMPACTS OF THE TROPICAL PACIFIC COUPLED PROCESS ON THE INTERANNUAL VARIABILITY IN THE INDIAN OCEAN".JOURNAL OF TROPICAL METEOROLOGY 16.3(2010):271-279. |
入库方式: OAI收割
来源:海洋研究所
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