| Impacts of Previous Winter Kuroshio SSTA on Summer Rainfall in China |
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| 引用本文： | LI Zhongxian,SUN Zhaobo,NI Donghong,ZENG Gang. Impacts of Previous Winter Kuroshio SSTA on Summer Rainfall in China[J]. , 2005, 19(1): 76-82 |
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| 作者姓名： | LI Zhongxian SUN Zhaobo NI Donghong ZENG Gang |
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| 作者单位： | Key Laboratory of Meteorological Disaster and Environmental Variation (KLME)，Nanjing University of Information Science & Technology，Nanjing 210044，Key Laboratory of Meteorological Disaster and Environmental Variation (KLME)，Nanjing University of Information Science & Technology，Nanjing 210044，Key Laboratory of Meteorological Disaster and Environmental Variation (KLME)，Nanjing University of Information Science & Technology，Nanjing 210044，Key Laboratory of Meteorological Disaster and Environmental Variation (KLME)，Nanjing University of Information Science & Technology，Nanjing 210044 |
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| 基金项目： | This study is supported by the National Natural Science Foundation of China under No. Grant 40175023 and by the GradateEducation and Innovation Project of Jiangsu Province: No. E30000008098-2. |
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| 摘 要： | 1. IntroductionAs well known, Kuroshio is a famous and strongwest boundary current in the North Pacific. It trans-fers enormous energy from the low latitudes to themid-high latitudes and releases huge heat flux to theatmosphere above (Hsiung, 1985). The variation ofKuroshio exerts great influence on weather and cli-mate in East Asian.During 1950-60s, Lü (1950, 1964) found that thewestern North Pacific SSTA had a close relation withsummer rainfall in China. In the 1970s, evidencesshowed…
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| 收稿时间： | 2004-03-30 |
| 修稿时间： | 2004-08-31 |
Impacts of Previous Winter Kuroshio SSTA on Summer Rainfall in China |
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| LI Zhongxian SUN Zhaobo NI Donghong ZENG Gang. Impacts of Previous Winter Kuroshio SSTA on Summer Rainfall in China[J]. Acta Meteorologica Sinica, 2005, 19(1): 76-82 |
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| Authors: | LI Zhongxian SUN Zhaobo NI Donghong ZENG Gang |
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| Abstract: | The relationship of Kuroshio sea surface temperature anomaly (SSTA) in the previous winter and sum- mer rainfall in China was analyzed based on observational studies and numerical simulations. Observational results indicate that there is a close relation between Kuroshio SSTA and precipitation in China. When Kuroshio SSTA is positive, the western Pacific subtropical high will be stronger and extend farther west- ward in the following summer, with Asian summer monsoon weaker and the frontal precipitation further southward. As a result, summer precipitation increases (decreases) in the mid-lower reaches of the Yangtze River (in North and Northeast China), and vice versa. Conclusions drawn by NCAR-CCM3 testify the observational results. |
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| Keywords: | winter Kuroshio SSTA East Asian summer monsoon precipitation in China numerical simulation transfer |
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