青藏高原山地湖泊扩涨与山地关系分析

qiang

青藏高原山地湖泊扩涨与山地关系分析

胡忠　 贾玉连　 张海荣　 张彪　 魏灵　

摘　要：基于1:10万与1:50万地形图,考察了青藏高原的山地湖泊及其流域的河流(水文)、雪线、冰川高度、各高度山地面积与湖泊面积之间的关系.高原湖泊的规模与流域山地(其高度,中、西部湖拔大于500～750 m,东部大于250m)存在密切关系.揭示山地降水是湖泊水的主要来源,其质(低温)与量是维持湖泊一定规模与稳定存在的主要因素.由于山地湖泊存在这种特殊的水文特点,因此,地质历史时期的暖湿期,高原山地湖泊比之低地、丘陵湖泊,扩涨规模可能更为显著.40～23 ka B.P,高原山地湖泊异乎寻常地扩涨,可能是降水在暖期季风雨增加时,在山地区增高更甚,更多的低温水流贮湖泊造成的.
关键词：青藏高原;山地湖泊;山地降水;湖泊扩涨
分类号：P512.32 　文献标识码：A
文章编号：1000-3657(2008)01-0144-06

Relationship between the expansion of mountain lakes and their catchment mountains on the Qinghai-Tibet Plateau

HU Zhong　 JIA Yu-lian　 ZHANG Hai-rong　 ZHANG Biao　 WEI Ling　



基金项目：国家自然科学基金项目(40401006)资助.
作者简介：胡忠,男,1961年生,副教授,主要从事地质地貌学的教学与科研工作,E-mail:hu221188@hotmail.com.
作者单位：胡忠（江西师范大学地理环境学院,江西,南昌,330026）　
　　　　　贾玉连（江西师范大学地理环境学院,江西,南昌,330026）　
　　　　　张海荣（惠州市惠阳区中山中学,广东,惠州,516211）　
　　　　　张彪（江西师范大学地理环境学院,江西,南昌,330026）　
　　　　　魏灵（南京大学海岸与海岛开发教育部重点实验室,江苏,南京,210008）　

参考文献：

[1]于革.全球晚第四纪湖泊数据库的研究[J].湖泊科学,1997,9(3):193-202.Yu Ge.Studies on global late Quaternary lake-level data bases[J].Journal of Lake Science,1997,9(3):193-202(in Chinese with English abstract).
[2]秦伯强.气候变化对亚洲内陆湖泊的影响研究-过去、现在与未来[D].中国科学院博士研究生毕业论文,1993:60-61.Qin Boqiang.Study on the impact of climate change on the Asian inland lakes--past,present and future[D].Ph.D.Dissertation of Chinese Academy of Sciences,1993:60-61(in Chinese with English abstract).
[3]范云崎.西藏内陆湖泊补给系数的初步探讨[J].海洋与湖沼,1983,14(2):118-127.Fan Yunqi.Preliminaw research on closed lake supply coefficient in Xizang[J].Oceanologia et Limnologia Sinica,1983,14(2):118-127(in Chinese with English abstract).
[4]Prell W L,lmbire J,Martimon D G,et al.Graphic correlation of oxygen isotope stratigraphy application to the late Quaternary[J].Paleoceanography,1986,1(2):137-162.
[5]黄赐璇,张青松,刘福涛.西藏日土县班公错地区晚更新世植物群与古气候探讨[J].自然资源学报,1989,4(3):247-253.Huang Cixuan,Zhang Qingsong,Liu Futao.Study on late Pleistocene climate change and flora in Bangong Co region,Rim county,Xiang[J].Journal of Natural Pesources,1989,40):247-253(in Chinese with English abstract).
[6]李世杰,郑本兴,焦克勤.西昆仑山南坡湖泊沉积演化的初步研究[J].地理科学,1991,11(4):306-313.Li shijie,Zheng Benxing,Jiao Keqin.Preliminary research on lakes evolution of the southern slope of West Kunlun Mountains[J].Scientia Geographica Sinica,1991,11(4):306-313(in Chinese with English abstract).
[7]胡东生.可可西里地区湖泊演化[J].干旱区地理,1995,18(1):60-67.Hu Dongsheng.Lakes evolution in Kekexili region[J].Arid Land Geography,1995,18(1):60-67(in Chinese with English abstract).
[8]陈克造,Bowler J M,Kelts K.四万年来青藏高原的气候变迁[J].第四纪研究,1990,10(1):21-31.Chen Kezao,Bowler J M,Kelts K.Climate change since 40 kaBP in Qingzang plateau[J].Quaternary Sciences,1990,10(1):21-31(in China with English abstract).
[9]郑绵平,刘俊英,齐文.从盐湖沉积探讨40 kaBP以来青藏高原古气候演替[C]//郑绵平.盐湖资源环境与全球变化.北京:地质出版社,1996:6-20.Zheng Mianping,Liu Junying,Qi Wen.Climate change research based on salt sedimentary stratigraphy during the last 40ka in Xizang Plateau[C]//Zheng Mianping.Salt Resource and Environment and Global Change.Beijing:Geological Publishing Housse.1996:6-20(in Chinese with English abstract).
[10]赵希涛,朱大岗,严富华,等.西藏纳木错末次间冰期以来的气候变迁与湖面变化[J].第四纪研究,2003,23(1):41-52.Zhao Xitao,Zhu Dagang,Yah Fuhua,et al.Climatic change and lake-level variation of Nam co,Xizang since the last interglacial stage[J].Quaternary Sciences,2003,23(1):41-52(in Chinese with English abstract).
[11]贾玉连,王苏民,吴艳宏,等.24 kaBP以来青藏高原中部湖泊演化及古降水量研究一以兹格塘错与错鄂为例[J].海洋与湖沼,2003,23(5):283-294.Jia Yulian,Wang Shuming.Wu Yanhong.et al.Preliminnary stuay of lake evolution and precipitation of Zigetang Co and Coe basins,central Qinghai-Xizang plateau,since 24 ka B.P[J].Oceanologia et Limnologia Sinica,2003,23(5):283-294(in Chinese with English abstract).
[12]李炳元.青藏高原环境演变的主要表征一湖泊演化[C]//施雅风,李吉均.青藏高原晚新生代的隆升与环境变化.广州:广东科技出版社,1998:331-372.Li Bingyuan.Lake evolution--the main characteristics of environmental change in Xizang Plateau[C]//Uplift and Environment Change during Late Caenozoic Era in Xizang Plateau(eds.Shi Yafeng,Li Jijun,Li Bingyuan).Guangzhou:Guangdong Science and Technology Press.1998:331-372(in Chinese with English abstract).
[13]Wang Fubao.Climatic changes in the Qinghai-Xizang(Tibetan)region of China during the Holocene[J].Quaternary Research,1987,28(4):50-60.
[14]郑绵平,向军.青藏高原盐湖[M].北京:北京科学技术出版社,1989:120-353.Zheng Mianping,Xiang Jun.Salt Lake in Xizang Plateau[M].Beijing:Beiing Science and Technology Press,1989:120-353(in Chinese with English abstract).
[15]Gasse F,el:al.A 13000-year climate record from Western Tibet[J].Nature,1991,353(24):742-745.
[16]中国科学院青藏高原综合科学考察队.西藏第四纪地质[M].北京:科学出版社,1983:1-251.Comprehensive Science Expedition in Xizang Plateau from Chinese Academy of Sciences.Quaternary Geology in Xizang[M].Beijing:Science Press,1983:1-251(in Chinese with English abstract).
[17]李栓科.中昆仑山区封闭湖泊湖面波动及其气候意义[J].湖泊科学,1992,4(1):19-30.Li Shuaike.Closed lakes level variation and their implications in middle Kunlun Mountains[J].Journal of Lake Sciences,1992,4(1):19-30(in Chinese with English abstract).
[18]Fonte J C,Melieres F,Gibert E,et al.Stable isotope and radiocarbon balances of two Tibetan hkes(SamxiCo,LongrnuCo)from 13000 BP[J].Quatermry Science tkeviews,1993,12:875-887.
[19]李炳元.青藏高原大湖期[J].地理学报,2000,55(2):174-181.Li Bingyuan.The last greatest lakes[J].Acta Geographica Sinica,2000,55(2):174-181(in Chinese with English abstract).
[20]朱大岗,孟宪刚,赵希涛,等.西藏纳木错和藏北高原古大湖晚更新世以来的湖泊演化与气候变迁[J].中国地质,2004,31(3):269-277.Zhu Dagang,Meng Xiangang,Zhao XJtao,el al.Evolution and climatic change of Nam Co of Tibet and ancient large lake in the northern Tibetan Plateau since the hte Pleistocene[J].Geology in China,2004,31(3):269-277(in Chinese with English abstract).
[21]Shi Yafeng,Yu Ge,Liu X D,et al,Reconstruction of the 40-30 kaBP enhanced India Monsoon climate based on geological records from the Tibetan Plateau[J].Palaeogeography Palaeoclimatology Palaeoecology,2001,169(1):742-745.
[22]施雅风,贾玉连,于革,等.40-30 KaBP青藏高原及邻区高温大降水事件的特征、影响及原因探讨[J].湖泊科学,2002,14(1):1-11.Shi Yafeng,Jia Yulian,Ge Yu,et al.Features,impacts and Causes of the high temperature and large precipitation event in the Tibetan Plateau and its adjacent area during 40-30 kaBP[J].Journal of Lake Science,2002,14(1):1-11(in Chinese with English abstract).
[23]于革,赖格英,刘健,等.MIS 3晚期典型阶段气候模拟的初步研究[J].第四纪研究,2003,23(1):12-24.Ge Yu.Lai Geying,Jian Liu,et al.Late MIS 3 climate simulations[J].Quaternary Sciences,2003,23(1):12-24(in Chinese with English abstract

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