| Qian Yongfu.The effects of different sea surface temperature distributions over the western Pacific on the summer monsoon properties[J].Acta Oceanologica Sinica,1993,(4):535-547 |
| The effects of different sea surface temperature distributions over the western Pacific on the summer monsoon properties |
| The effects of different sea surface temperature distributions over the western Pacific on the summer monsoon properties |
| 投稿时间：1992-12-15 修订日期：1993-02-04 |
| DOI： |
| 中文关键词: Sea surface temperature anomaly monsoon climate modelling computational models of SST |
| 英文关键词:Sea surface temperature anomaly monsoon climate modelling computational models of SST |
| 基金项目:Supported by the National Fundamental Key Research:"studies on climate dynamics and climate prediction theory." |
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| 摘要点击次数: 808 |
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| 中文摘要: |
| A modified and improved primitive equation numerical model with p-sigma incorporated vertical coordinates is used to simulate the effects of different sea surface temperature distributions over the western Pacific on the summer monsoon properties.The different sea surface temperature (SST) distributions are automatically generated in the time integrations by using two different SST models, one of which is called the deep ocean model (DOM) and the other the shallow ocean model (SOM).The SST generated by the DOM has the distribution pattern of the initial SST which is similar to the pattern in the cold water years over the western Pacific, while the SST generated by the SOM has the pattern similar to that in the warm water years.The differences between the experimental results by using DOM and SOM are analyzed in detail. |
| 英文摘要: |
| A modified and improved primitive equation numerical model with p-sigma incorporated vertical coordinates is used to simulate the effects of different sea surface temperature distributions over the western Pacific on the summer monsoon properties.The different sea surface temperature (SST) distributions are automatically generated in the time integrations by using two different SST models, one of which is called the deep ocean model (DOM) and the other the shallow ocean model (SOM).The SST generated by the DOM has the distribution pattern of the initial SST which is similar to the pattern in the cold water years over the western Pacific, while the SST generated by the SOM has the pattern similar to that in the warm water years.The differences between the experimental results by using DOM and SOM are analyzed in detail. |
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