| 近千年中国东部夏季雨带位置的变化 |
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| 引用本文： | 黄建斌,王绍武. 近千年中国东部夏季雨带位置的变化[J]. 气候变化研究进展, 2007, 3(Z1): 19-25 |
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| 作者姓名： | 黄建斌 王绍武 |
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| 作者单位： | Huang Jianbin（Department of Atmospheric Science, School of Physics, Peking University, Beijing 100871, China） Wang Shaowu（Department of Atmospheric Science, School of Physics, Peking University, Beijing 100871, China） |
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| 摘 要： | Based on the variations of geographical locations, the summer rain belts over eastern China were classified in this study into eight types: Inner Mongolia, North China, the Yellow River, the Huaihe River, the Yangtze River, the northern and southern parts of Jiangnan ( to the south of the lower Yangtze River valley), and South China. The file of 8-type rain belts was compiled from 1470 to 2005, and in order to extend the file of rain belts, it was further merged into a file of 4-type rain belts and also completed during the last millennium from 1000 to 1999. At last, the two files show that summer rain belts frequently occur in the Yangtze River valley in warm climate periods, but in the Yellow River or the Huaihe River valley in cold periods.
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| 关 键 词： | last millennium eastern China rain belt |
| 文章编号： | 1673-1719(2007)Suppl.-0019-07 |
| 修稿时间： | 2006-09-13 |
Variations of Geographical Latitude of Summer Rain Belts over Eastern China During the Last Millennium |
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| Huang Jianbin,Wang Shaowu. Variations of Geographical Latitude of Summer Rain Belts over Eastern China During the Last Millennium[J]. Progressus Inquisitiones DE, 2007, 3(Z1): 19-25 |
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| Authors: | Huang Jianbin Wang Shaowu |
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| Abstract: | Based on the variations of geographical locations, the summer rain belts over eastern China were classified in this study into eight types: Inner Mongolia, North China, the Yellow River, the Huaihe River, the Yangtze River, the northern and southern parts of Jiangnan ( to the south of the lower Yangtze River valley), and South China. The file of 8-type rain belts was compiled from 1470 to 2005, and in order to extend the file of rain belts, it was further merged into a file of 4-type rain belts and also completed during the last millennium from 1000 to 1999. At last, the two files show that summer rain belts frequently occur in the Yangtze River valley in warm climate periods, but in the Yellow River or the Huaihe River valley in cold periods. |
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| Keywords: | last millennium eastern China rain belt |
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