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  • CN 62-1070/P
  • ISSN 1000-694X
  • Bimonthly 1981
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Future Trend Characteristics of Hydrological Time Series in the Weiganhhe River Basin

  • Li Rui ,
  • Zhang Fei ,
  • Gao Yuxiao ,
  • Zhou Mei ,
  • Li Xiaohang ,
  • Wang Dongfang
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  • 1. College of Resources and Environment Science, Xinjiang University, Urumqi 830046, China;
    2. Key Laboratory of Oasis Ecology under Ministry of Education, Xinjiang University, Urumqi 830046, China;
    3. General Institutes of Higher Learning Key Laboratory of Smart City and Environmental Modeling, Xinjiang University, Urumqi 830046, China

Received date: 2015-03-24

  Revised date: 2015-06-21

Abstract

Every river system has its own unique flow variation. In this paper, we discussed the problem of the R/S and Mann-Kendall method used in hydrological time series, and presented a method of the combination of R/S and Mann-Kendall to analyze future trend characteristics of hydrological time series, taking the Langan Reservoir Station, Heizi Reservoir Station, Thousand Buddha Cave (synthetic) Reservoir Station as examples. The results show that:the Hearst index for the three stations were all less than 0.5, UFk were all more than 0, indicating a significant decline flow in future.

Cite this article

Li Rui , Zhang Fei , Gao Yuxiao , Zhou Mei , Li Xiaohang , Wang Dongfang . Future Trend Characteristics of Hydrological Time Series in the Weiganhhe River Basin[J]. Journal of Desert Research, 2016 , 36(6) : 1713 -1720 . DOI: 10.7522/j.issn.1000-694X.2015.00095

References

[1] Arthington A H,Tharme R E,Brizga S O,et al.Environmental flow Assessment with Emphasison Holistic Methodologies[C].Proceedings of the Second International Symposium on the Management of Large Rivers for Fisheries Volume Ⅱ,Phnom Penh,Cambodia.2004.
[2] 杨涛,李怀恩,张亚平,等.渭河宝鸡市区段河道生态基流量初步研究[J].水资源与水工程学报,2007,18(5):17-23.
[3] 李翀,廖文根,彭静,等.宜昌站1900-2004年生态水文特征变化[J].长江流域资源与环境,2007,16(1):76-80.
[4] 王文圣,丁晶,李跃清.水文小波分析[M].北京:化学工业出版社,2005.
[5] 芮孝芳.水文学原理[M].北京:中国水利水电出版社,2005.
[6] 张建云,宋晓猛,王国庆,等.变化环境下城市水文学的发展与挑战——Ⅰ.城市水文效应[J].水科学进展,2014,25(4):594-605.
[7] 张军以,王腊春,苏维词,等.岩溶地区人类活动的水文效应研究现状及展望[J].地理科学进展,2014,33(8):1125-1135.
[8] Liu L C,Song Y X,Gao Y H,et al.Effects of micro biotic crusts on evaporation from the revegetated area in a Chinese desert[J].Australian Journal of Soil Reasearch,2007,45(6):422-427.
[9] Zhou Y,Persand N,Wang H.Scale invariance of daily runoff time series in agricultural watersheds[J].Hydrology and Earth System Sciences,2006,10:79-91.
[10] 王孝礼,胡宝清,夏军.水文时序趋势与变异点的R/S分析[J].武汉大学学报:工学版,2002,35(2):10-12.
[11] 曲广周,覃英宏,刘亮,等.基于R/S分析黄河及黄土高原主要河流水资源的变化[J].中国沙漠,2010,30(2):467-470.
[12] Lins H F,Slack J R.Stream flow trends in the United States[J].Geophysical Research Letters,1999,26(2):227.
[13] Sneyers R.On the statistical analysis of series of observations[J].Journal of Biological Chemistry,1991,258(22):13680-13684.
[14] Kendall M G.Rank Correlation Methods[M].London,UK:Charles Griffin,1975:202-206.
[15] 艾萍,吴军澜,王雪娇,等.基于Mann-Kendall法的水温时间序列检验[J].水利水电技术,2014,45(2):10-13.
[16] 于延胜,陈兴伟.基于Mann-Kendall法的径流丰枯变化过程划分[J].水资源与水工程学报,2013,24(1):60-61.
[17] Kimpet I,Mandabu D.Yamanaka Y,et al.Precipitation in N.C pell between 1987 and 1996[J].International Journal of Climatology,2007,15(2):245-256.
[18] 徐宗学,张楠.黄河流域近50年降水变化趋势分析[J].地理研究,2006,25(1):27-35.
[19] 刘美萍,哈斯.中全新世以来查干淖尔古湖面波动[J].中国沙漠,2015,35(2):306-312.
[20] 徐浩杰,杨太保,柴绍豪.1961-2010年讨赖河山区径流变化特征及其驱动因素[J].中国沙漠,2014,34(3):878-884.
[21] 华婷,王训明,郎丽丽,等.甘肃省气温与降水变化趋势及其对主要流域径流量的影响[J].中国沙漠,2015,35(3):744-752.
[22] 满苏尔·沙比提,胡江玲.新疆渭干河-库车河三角洲绿洲地下水特征对天然植被的影响分析[J].冰川冻土,2010,32(2):422-428.
[23] 乔旭宁,杨永菊,杨德刚.生态服务功能价值空间转移评价——以渭干河流域为例[J].中国沙漠,2011,31(4):1008-1004.
[24] 霍金炜,杨德刚,张新焕.基于农业节水的干旱区绿洲可持续发展研究——以渭干河流域为例[J].中国沙漠,2013,33(1):295-301.
[25] 王生霞,叶柏生,周兆叶,等.基于NDVI分析渭干河流域绿洲耗水对地表径流的影响[J].草业科学,2013,30(4):487-494.
[26] 丁晶,邓育仁.随机水文学[M].成都:成都科技大学出版社,1988.
[27] 法尔科内.分形几何数学基础及其应用[M].北京:人民邮电出版社,2007.
[28] 覃基爱,陈雪英,郑艳霞.宜昌径流时间序列的统计分析[J].水文,1993,13(5):15-21.
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