STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

杨针娘; 胡鸣高

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STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

杨针娘, 胡鸣高

文章导航 > Chinese Geographical Science > 1993 > 3(1): 51-60

杨针娘, 胡鸣高. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. 中国地理科学, 1993, 3(1): 51-60.

引用本文:

杨针娘, 胡鸣高. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. 中国地理科学, 1993, 3(1): 51-60.

Yang Zhenniang, Woo Mingko. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. Chinese Geographical Science, 1993, 3(1): 51-60.

Citation:

Yang Zhenniang, Woo Mingko. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. Chinese Geographical Science, 1993, 3(1): 51-60.

STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

杨针娘¹,
胡鸣高²

1.
Lanzhou Institute of Glaciology and Geogryology, Chinese Academy of Sciences, Langzhou 730000, PRC;
2.
Department of Geography, McM aster University, Hamilton, Ontario, Canada

STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

Yang Zhenniang¹,
Woo Mingko²

1.
Lanzhou Institute of Glaciology and Geogryology, Chinese Academy of Sciences, Langzhou 730000, PRC;
2.
Department of Geography, McM aster University, Hamilton, Ontario, Canada

摘要: The eastern Qinghai-Xizang (Tibet) Plateau is the headwater area for many large Asian rivers. Permafrost occurs above 4,200 m a.s.l. and glaciers occupy the summits and high valleys of the east-west trending mountain chains. Annual runoff generally increases with precipitation which is augmented southward by the rise in topography. Rainfall, snow melt, glacier melt and groundwater are the primary sources of stream flow, and the presence of permafrost enhances the flashiness of runoff response to rainfall and snowmelt events. Peak flows are concentrated between June and September. And winter is low flow season. Three types of runoff patterns may be distinguished according to their primary sources of water supply: snowmelt and rainfall, glacier melt and snowmelt, and groundwater. Large rivers generally drain more than one environments and their runoff regime reflects an integration of the various flow patterns on the plateau.
- Qinghai-Xizang Plateau /
- permafrost /
- glacial melt runoff /
- specific runoff
Abstract: The eastern Qinghai-Xizang (Tibet) Plateau is the headwater area for many large Asian rivers. Permafrost occurs above 4,200 m a.s.l. and glaciers occupy the summits and high valleys of the east-west trending mountain chains. Annual runoff generally increases with precipitation which is augmented southward by the rise in topography. Rainfall, snow melt, glacier melt and groundwater are the primary sources of stream flow, and the presence of permafrost enhances the flashiness of runoff response to rainfall and snowmelt events. Peak flows are concentrated between June and September. And winter is low flow season. Three types of runoff patterns may be distinguished according to their primary sources of water supply: snowmelt and rainfall, glacier melt and snowmelt, and groundwater. Large rivers generally drain more than one environments and their runoff regime reflects an integration of the various flow patterns on the plateau.
- Qinghai-Xizang Plateau /
- permafrost /
- glacial melt runoff /
- specific runoff

[1]	Lixiang WEN, Meng GUO, Shuai YIN, Shubo HUANG, Xingli LI, Fangbing YU. Vegetation Phenology in Permafrost Regions of Northeastern China Based on MODIS and Solar-induced Chlorophyll Fluorescence . Chinese Geographical Science, 2021, 31(3): 459-473. doi: 10.1007/s11769-021-1204-x
[2]	WANG Rui, DONG Zhibao, ZHOU Zhengchao. Different Responses of Vegetation to Frozen Ground Degradation in the Source Region of the Yellow River from 1980 to 2018 . Chinese Geographical Science, 2020, 30(4): 557-571. doi: 10.1007/s11769-020-1135-y
[3]	WANG Shengting, SHENG Yu, LI Jing, WU Jichun, CAO Wei, MA Shuai. An Estimation of Ground Ice Volumes in Permafrost Layers in North-eastern Qinghai-Tibet Plateau, China . Chinese Geographical Science, 2018, 28(1): 61-73. doi: 10.1007/s11769-018-0932-z
[4]	HU Guojie, ZHAO Lin, LI Ren, WU Tonghua, WU Xiaodong, PANG Qiangqiang, XIAO Yao, QIAO Yongping, SHI Jianzong. Modeling Hydrothermal Transfer Processes in Permafrost Regions of Qinghai-Tibet Plateau in China . Chinese Geographical Science, 2015, 25(6): 713-727. doi: 10.1007/s11769-015-0733-6
[5]	LI Jing, SHENG Yu, WU Jichun, et al.. Modeling Regional and Local-scale Permafrost Distribution in Qinghai-Tibet Plateau Using Equivalent-elevation Method . Chinese Geographical Science, 2012, 22(3): 278-287.
[6]	LIU Xianzhao, LI Jiazhu. Application of SCS Model in Estimation of Runoff from Small Watershed in Loess Plateau of China . Chinese Geographical Science, 2008, 18(3): 235-241. doi: 10.1007/s11769-008-0235-x
[7]	JIN Huijun, SUN Guangyou, YU Shaopeng, JIN Rui, HE Ruixia. Symbiosis of Marshes and Permafrost in Da and Xiao Hinggan Mountains in Northeastern China . Chinese Geographical Science, 2008, 18(1): 62-69. doi: 10.1007/s11769-008-0062-0
[8]	CHEN Liqun, LIU Changming, LI Yanping, WANG Guoqiang. Impacts of Climatic Factors on Runoff Coefficients in Source Regions of the Huanghe River . Chinese Geographical Science, 2007, 17(1): 47-55. doi: 10.1007/s11769-007-0047-4
[9]	CHEN Hui, LI Shuang-cheng, ZHANG Yi-li. IMPACT OF ROAD CONSTRUCTION ON VEGETATION ALONGSIDE QINGHAI-XIZANG HIGHWAY AND RAILWAY . Chinese Geographical Science, 2003, 13(4): 340-346.
[10]	CHEN Jie, GONG Zi-tong, CHEN Zhi-cheng, TAN Man-zhi. CLASSIFICATION OF CRYOSOLS:SIGNIFICANCE, ACHIEVEMENTS AND CHALLENGES . Chinese Geographical Science, 2003, 13(4): 352-358.
[11]	王学全, 高前兆. THE PRECIPITATION INFILTRATION AND RUNOFF RECHARGING EXPERIMENT OBSERVATION IN THE TAKLIMAKAN DESERT . Chinese Geographical Science, 1999, 9(3): 284-288.
[12]	郑度, 李炳元. PROGRESS IN STUDIES ON GEOGRAPHICAL ENVIRONMENTS OF THE QINGHAI XIZANG PLATEAU . Chinese Geographical Science, 1999, 9(4): 289-296.
[13]	章新平. VARIATION OF d δ¹⁸O/dT IN PRECIPITATION IN THE QINGHAI-XIZANG PLATEAU . Chinese Geographical Science, 1997, 7(4): 328-338.
[14]	徐叔鹰, 潘保田. PALEOSOLS AND THEIR REFLECTION OF THE ENVIRONMENTAL CHANGES IN THE NORTHEAST REGION OF THE QINGHAI-XIZANG PLATEAU . Chinese Geographical Science, 1996, 6(1): 24-34.
[15]	朱林楠, 吴紫汪, 刘永智, 李东庆. PERMAFROST DEGENERATION IN THE EAST OF QINGHAI-XIZANG PLATEAU . Chinese Geographical Science, 1996, 6(3): 231-238.
[16]	杨针娘. GLACIER MELTWATER RUNOFF IN CHINA AND ITS NOURISHMENT TO RIVER . Chinese Geographical Science, 1995, 5(1): 66-76.
[17]	王绍令. PERMAFROST　CHANGES　AND　ENVIRONMENTAL　PROBLEMS　ALONG　THE　QINGHAI－XIZANG　HIGHWAY . Chinese Geographical Science, 1995, 5(2): 149-156.
[18]	刘天仇. STUDIES ON WATER STAGE FLUCTUATION OF YAMZHO LAKE IN XIZANG . Chinese Geographical Science, 1995, 5(4): 344-354.
[19]	施雅风, 郑本兴, 李士杰. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS . Chinese Geographical Science, 1992, 2(4): 293-311.
[20]	李恒, 武素功. THE FLORISTIC STRUCTURE OF THE XIZANG PART OF THE QINGHAI-XIZANG PLATEAU PLANT SUBKINGDOM . Chinese Geographical Science, 1991, 1(3): 221-233.

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STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

杨针娘¹,
胡鸣高²

1. Lanzhou Institute of Glaciology and Geogryology, Chinese Academy of Sciences, Langzhou 730000, PRC;

2. Department of Geography, McM aster University, Hamilton, Ontario, Canada

刊出日期: 1993-03-20

关键词:

Qinghai-Xizang Plateau /

permafrost /

glacial melt runoff /

specific runoff

摘要: The eastern Qinghai-Xizang (Tibet) Plateau is the headwater area for many large Asian rivers. Permafrost occurs above 4,200 m a.s.l. and glaciers occupy the summits and high valleys of the east-west trending mountain chains. Annual runoff generally increases with precipitation which is augmented southward by the rise in topography. Rainfall, snow melt, glacier melt and groundwater are the primary sources of stream flow, and the presence of permafrost enhances the flashiness of runoff response to rainfall and snowmelt events. Peak flows are concentrated between June and September. And winter is low flow season. Three types of runoff patterns may be distinguished according to their primary sources of water supply: snowmelt and rainfall, glacier melt and snowmelt, and groundwater. Large rivers generally drain more than one environments and their runoff regime reflects an integration of the various flow patterns on the plateau.

English Abstract

杨针娘, 胡鸣高. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. 中国地理科学, 1993, 3(1): 51-60.

引用本文:

杨针娘, 胡鸣高. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. 中国地理科学, 1993, 3(1): 51-60.

Yang Zhenniang, Woo Mingko. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. Chinese Geographical Science, 1993, 3(1): 51-60.

Citation:

Yang Zhenniang, Woo Mingko. STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU[J]. Chinese Geographical Science, 1993, 3(1): 51-60.

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STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

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出版历程

STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

1. Lanzhou Institute of Glaciology and Geogryology, Chinese Academy of Sciences, Langzhou 730000, PRC; 2. Department of Geography, McM aster University, Hamilton, Ontario, Canada

English Abstract

STREAMFLOW CHARACTERISTICS OF THE EASTERN QINGHAI-XIZANG PLATEAU

1. Lanzhou Institute of Glaciology and Geogryology, Chinese Academy of Sciences, Langzhou 730000, PRC; 2. Department of Geography, McM aster University, Hamilton, Ontario, Canada

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目录

1. Lanzhou Institute of Glaciology and Geogryology, Chinese Academy of Sciences, Langzhou 730000, PRC;

2. Department of Geography, McM aster University, Hamilton, Ontario, Canada

1. Lanzhou Institute of Glaciology and Geogryology, Chinese Academy of Sciences, Langzhou 730000, PRC;

2. Department of Geography, McM aster University, Hamilton, Ontario, Canada