| 近四十年我国气候变化的初步分析 |
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| 引用本文： | 陈隆勋,邵永宁,张清芬 任阵海 田广生.近四十年我国气候变化的初步分析[J].应用气象学报,1991,2(2):164-174. |
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| 作者姓名： | 陈隆勋 邵永宁 张清芬 任阵海 田广生 |
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| 作者单位： | 1.国家气象局气象科学研究院
(陈隆勋，邵永宁，张清芬)，国家环保局环境科学院
(任阵海)，国家环保局环境科学院(田广生) |
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| 摘 要： | 本文对近四十年来我国的气候变化作了一个初步分析。结果表明，众所周知的全球增暖在我国只反映在东北、华北和西北西部地区；大约35°N以南，南岭以北，青藏高原以东地区是变冷区，变冷中心在四川、陕南和滇北；在全球温室效应下，高低纬变湿和中纬变干，而我国则大部分地区变干，华北和西北变干更明显。我国气候变化特点和全球增暖趋势有许多不一致，这一点值得引起我国气候学家的注意。
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Preliminary Analysis of Climatic Change During the Last 39 Years in China |
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| Affiliation: | 1) (Academy of Meteorological Science, SMA); 2) (Academy of Environment Science, National Environment and Protection Agency, Beijing) |
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| Abstract: | The preliminary analysis of climatic change in China during the last 39 years has been made in this paper. The results show that although the global climate is getting warmer, some parts of China are cooling. The warming only occurs in northeast, north and west part of northwest China while the areas between about 35oN and Nanling mountain, east of Tibetan Plateau in China are getting cooler. The cooling centers are located in Sichuan, the south part of Shanxi and the north part of Yunnan, respectively. Under the greenhouse effect, the precipitation becomes more in low and high latitudes and less in middle latitude. But, the precipitation in the most parts of China becomes less, especially in north and northwest China |
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