[1]李勃,穆兴民,高鹏,等.1956-2017年黄河干流径流量时空变化新特征[J].水土保持研究,2019,26(06):120-126,132.
 LI Bo,MU Xingmin,GAO Peng,et al.New Characteristics of Temporal and Spatial Changes of Runoff in the Mainstream of Yellow River from 1956 to 2017[J].Research of Soil and Water Conservation,2019,26(06):120-126,132.
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1956-2017年黄河干流径流量时空变化新特征

参考文献/References:

[1] Zhang Q, Singh V P, Sun P, et al. Precipitation and streamflow changes in China:Changing patterns, causes and implications[J]. Journal of Hydrology,2011,410(3/4):204-216.
[2] Mcmahon T A, Vogel R M, Peel M C, et al. Global streamflows. Part 1:Characteristics of annual streamflows[J]. Journal of Hydrology, 2007,347(3):243-259.
[3] Milly P C D, Dunne K A, Vecchia A V. Global pattern of trends in streamflow and water availability in a changing climate[J]. Nature, 2005,438(7066):347-350.
[4] Pachauri R K. Climate change 2007:Synthesis report. Contribution of working groups I, Ⅱ and Ⅲ to the fourth assessment report[J]. Speculum, 2007,77(2):586-588.
[5] Milliman J D, Farnsworth K L, Jones P D, et al. Climatic and anthropogenic factors affecting river discharge to the global ocean, 1951-2000[J]. Global & Planetary Change, 2008,62(3):187-194.
[6] 陈敏建,王浩,王芳.内陆干旱区水分驱动的生态演变机理[J].生态学报,2004,24(10):2108-2114.
[7] 陈霁巍,穆兴民.黄河断流的态势、成因与科学对策[J].自然资源学报,2000,15(1):31-35.
[8] Mu X M, Zhang L, McVicar T R. Analysis of the impact of conservation measures on stream flow regime in catchments of the Loess Plateau, China[J]. Hydrological Processes, 2007,21(16):2124-2134.
[9] 田景环,崔庆,徐建华,等.黄河流域大中型水库水面蒸发对水资源量的影响[J].山东农业大学学报:自然科学版,2005,36(3):391-394.
[10] 张建云,章四龙,王金星,等.近50年来中国六大流域年际径流变化趋势研究[J].水科学进展,2007,18(2):230-234.
[11] 刘昌明,成立.黄河干流下游断流的径流序列分析[J].地理学报,2000,55(3):257-265.
[12] 刘昌明,张学成.黄河干流实际来水量不断减少的成因分析[J].地理学报,2004,59(3):323-330.
[13] 赵玉,穆兴民,何毅,等.1950-2011年黄河干流水沙关系变化研究[J].泥沙研究,2014(4):32-38.
[14] 赵广举,穆兴民,田鹏,等.近60年黄河中游水沙变化趋势及其影响因素分析[J].资源科学,2012,34(6):1070-1078.
[15] 孙洋洋,穆兴民,高鹏,等.黄河上中游区径流量格局长期变化过程[J].水土保持研究,2017,24(3):59-64.
[16] 张晓萍,张橹,王勇,等.黄河中游地区年径流对土地利用变化时空响应分析[J].中国水土保持科学,2009,7(1):19-26.
[17] 许炯心.人类活动对黄河河川径流的影响[J].水科学进展,2007,18(5):648-655.
[18] 李二辉,穆兴民,赵广举.1919-2010年黄河上中游区径流量变化分析[J].水科学进展,2014,25(2):155-163.
[19] 穆兴民,高鹏,巴桑赤烈,等.应用流量历时曲线分析黄土高原水利水保措施对河川径流的影响[J].地球科学进展,2008,23(4):382-389.
[20] 张小苗,穆兴民,赵广举,等.基于极端日流量的延河径流变化特征研究[J].人民黄河,2018,40(8):12-18.
[21] 穆兴民.黄土高原生态水文研究[M].北京:中国林业出版社,2001:34-47.
[22] 毕彩霞,穆兴民,赵广举,等.渭河流域气候变化与人类活动对径流的影响[J].中国水土保持科学,2013,11(2):33-38.
[23] 姚文艺,冉大川,陈江南.黄河流域近期水沙变化及其趋势预测[J].水科学进展,2013,24(5):607-616.
[24] 宋小燕.松花江流域水沙演变及其对人类活动的响应[D].陕西杨凌:中国科学院水土保持研究所,2010.
[25] Gao P, Geissen V, Ritsema C J, et al. Impact of climate change and anthropogenic activities on stream flow and sediment discharge in the Wei River basin, China[J]. Hydrology & Earth Systemences, 2012,17(3):961-972.
[26] Pettitt A N. A non-parametric approach to the change-point problem[J]. Journal of the Royal Statistical Society, 1979,28(2):126-135.
[27] 穆兴民,李靖,王飞,等.黄河天然径流量年际变化过程分析[J].干旱区资源与环境,2003,17(2):1-5.
[28] 史红玲,胡春宏,王延贵,等.黄河流域水沙变化趋势分析及原因探讨[J].人民黄河,2014,36(4):1-5.
[29] 李伟珮,闫观清,李保国,等.黄河流域近300年来水文情势及其变化[J].人民黄河,2009,31(11):25-26.
[30] 黄河水利科学研究院.黄河水沙变化趋势与水利枢纽工程建设对黄河健康的影响[R].郑州:黄河水利科学研究院,2007.

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备注/Memo

收稿日期:2018-12-10;改回日期:2019-01-15。
基金项目:国家重点研发计划"黄河流域水沙多时空演变及其分异规律"(2016YFC0402401);黄土高原土壤侵蚀与旱地农业国家重点实验室专项经费"黄河水沙多时空演变及驱动机制"(A314021403-Q2)
作者简介:李勃(1995-),女,陕西绥德人,硕士研究生,研究方向为水土保持和生态水文。E-mail:2498257968@qq.com
通讯作者:赵广举(1980-),男,河南驻马店人,博士,研究员,主要从事流域水文过程与土壤侵蚀模拟研究。E-mail:gjzhao@ms.iswc.ac.cn

更新日期/Last Update: 1900-01-01