| 引用本文: | 施雅风.21kaBP青藏高原有远高于现代降水量的可能性吗?.湖泊科学,2000,12(2):165-166. DOI:10.18307/2000.0210 |
| SHI Yafeng.Is really the Higher Precipitation occured during 21kaBP on the Tibetan Plateau. J. Lake Sci.2000,12(2):165-166. DOI:10.18307/2000.0210 |
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| 21kaBP青藏高原有远高于现代降水量的可能性吗? |
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施雅风1,2
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1.中国科学院寒区旱区环境与工程研究所, 兰州730000;2.中国科学院南京地理与湖泊研究所, 南京210008
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| 摘要: |
| 作者认为，青藏高原21kaBP不可能存在远高于现代降水量的可能性，对陈星等发表在《湖泊科学》（2000)的论文进行了质疑。 |
| 关键词: 21kaBP 气候模拟；青藏高原；季风 |
| DOI：10.18307/2000.0210 |
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| Is really the Higher Precipitation occured during 21kaBP on the Tibetan Plateau |
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SHI Yafeng
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Cold and Arid Regions Environmental and Engineering Research Institute,CAS
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| Abstract: |
| The author thinks that there was no Higher Precipitation occured during 21kaBP on the Tibetan Plateau,which was suggested by Chen Xing et al(2000) in this issue. |
| Key words: 21kaBP climate simulation Tibetan Plateau,monsoon |
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