| 引用本文: | 于革,陈星,薛滨.对《21ka BP青藏高原有远高于现代降水量的可能性吗》的回复.湖泊科学,2000,12(2):167-170. DOI:10.18307/2000.0211 |
| YU Ge,CHEN Xing,XUE Bin.Reply to "Is really the Higher Precipitation occurred during 21kaBP on the Tibetan Plateau?". J. Lake Sci.2000,12(2):167-170. DOI:10.18307/2000.0211 |
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| 对《21ka BP青藏高原有远高于现代降水量的可能性吗》的回复 |
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于革, 陈星, 薛滨
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中国科学院南京地理与湖泊研究所湖泊沉积与环境开放实验室, 南京210008
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| 摘要: |
| 针对施雅风先生认为，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)的论文进行的质疑， 本文作者给予了正面答复。 |
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| DOI：10.18307/2000.0211 |
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| Reply to "Is really the Higher Precipitation occurred during 21kaBP on the Tibetan Plateau?" |
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YU Ge, CHEN Xing, XUE Bin
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Key Laboratory of Lake Sedimentation and Environment, Nanjing Institute of Geography & Limnology, CAS
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| Abstract: |
| The authors give a reply to the debate by SHI Yafeng(2000) titled "Is really the Higher Precipitation occurred during 21kaBP on the Tibetan Plateau?" in Journal of Lake Sciences |
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