This paper makes use of the monthly natural runoff data from1956 to 2000, the monthly
air temperature data and precipitation data from 1956 to 2004 to analyze the evolution
characteristics of the runoff in the Yarlung Zangbo River basin in the later half of the 20th
century and the relation between runoff evolution and climatic change.The results show that the
interannual evolution of the runoff in the Yarlung Zangbo River basin is stable, but the intraannual
distribution of the runoff is extremely uneven, the maximum monthly runoff accounts for
30.1%, while the minimum runoff only accounts for 2.1%, and indication of the great difference
in the runoff between low water season and flood water season.The climate in the Yarlung
Zangbo River basin is calefactive, and the increasing trend of the precipitation is obvious, having
the same evolution periods with runoff.After elementary analysis of the decadal runoff in the
Yarlung Zangbo River basin, we found that the increase of the water supply is mainly controlled
by climate change, but is also affected by the changes of the earth surface conditions in the
basin and maybe a representation of the long period of variation of high and low stream flow.
Relevant data are required to validate and analyze this kind of periodic variations.
LIU Jian1, 2, YAO Zhi-jun1, CHEN Chuan-you1
. Evolution Tr end and Causation Analysis of the Runoff Evolution in the Yar lung Zangbo River Basin[J]. JOURNAL OF NATURAL RESOURCES, 2007
, 22(3)
: 471
-477
.
DOI: 10.11849/zrzyxb.2007.03.017
[1] 刘天仇.雅鲁藏布江水文特征[J].地理学报,1999,54:157~164.[LIU Tian-chou.Hydrological characteristics of Yalung ZangboRiver.Acta Geographica Sinica,1999,54:157- 164.]
[2] 胡兴林.黑河流域径流演变规律及区域性水资源优化配置分析[J].水文,2003,23(1):32~36.[HU Xing-lin.Analysis on runoffvariation regularity and regional water resources optimum allocation in the Heihe River basin.Hydrology,2003,23(1):32- 36.]
[3] 关志华,陈传友,等.西藏河流与湖泊[M].北京:科学出版社,1984.10~22.[GUAN Zhi-hua,CHEN Chuan-you.Rivers andLakes in Tibet.Beijing:Science Press,1984.10- 22.]
[4] 刘新春,杨青,梁云.近40 年阿克苏河流域径流变化特征及影响因素研究[J].中国人口资源与环境,2006,16(3):82~87.[LIU Xin-chun,YANG Qing,LIANG Yun.Study on the change of runoff and the effect factors in the Aksu River basin inrecent 40 years.China Population,Resources and Environment,2006,16(3):82- 87.]
[5] 苏珍,刘宗香,王文悌,等.青藏高原冰川对气候变化的响应及趋势预测[J].地球科学进展,1999,14(6):607~612.[SU Zhen,LIU Zong-xiang,WANG Wen-ti,et al.Glacier fluctuations responding to climate change and forecast of its tendency over theQinghai-Tibet Plateau.Advance in Earth Sciences,1999,14(6):607- 612.]
[6] 周顺武,张勇.近42 年雅鲁藏布江中游四季气温变化特征分析[J].成都气象学院学报,2000,15(4):307~311.[ZHOU Shunwu,ZHANG Yong.Analysis of seasonal temperature variation over middle reaches of Yalutsangpo River during past 42years.Journal of Chengdu Institute of Meteorology,2000,15(4):307- 311.]
[7] 葛朝霞,王会容,曹丽青,等.藏降水量、气温变化特征及相关关系[J].气象科学,2004,24(4):468~473.[GE Zhao-xia,WANGHui-rong,CAO Li-qing,et al.The change characteristics and correlativity of precipitation and air temperature in TibetRegion. Scientia Meteorologica Sinica,2004,24(4):468- 473.]