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 |
|
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。 |
关键词: |
DOI:10.18307/2000.0211 |
分类号: |
基金项目: |
|
Reply to "Is really the Higher Precipitation occurred during 21kaBP on the Tibetan Plateau?" |
YU Ge, CHEN Xing, XUE Bin
|
Key Laboratory of Lake Sedimentation and Environment, Nanjing Institute of Geography & Limnology, CAS
|
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 |
Key words: |