[1]潘彬,韩美,倪娟.黄河下游近50年径流量变化特征及影响因素[J].水土保持研究,2017,24(01):122-127.
　PAN Bin,HAN Mei,NI Juan.Characteristics and Influence Factors of Runoff Variation in the Lower Reaches of the Yellow River in the Last 50 Years[J].Research of Soil and Water Conservation,2017,24(01):122-127.
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黄河下游近50年径流量变化特征及影响因素

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 24 期数: 2017年01期 页码: 122-127 栏目: 出版日期: 2017-02-28
Title:
Characteristics and Influence Factors of Runoff Variation in the Lower Reaches of the Yellow River in the Last 50 Years
作者:
潘彬1, 韩美1, 倪娟2
1. 山东师范大学 地理与环境学院, 济南 250014;
2. 山东城建学院, 济南 250014
Author(s):
PAN Bin1, HAN Mei1, NI Juan2
1. School of geography and environment, Shandong Normal University, Ji’nan 250014, China;
2. Shandong Urban Construction Vocational College, Ji’nan 250014, China
关键词:
黄河下游; 降水量; 径流量; 人类活动
Keywords:
the lower reaches of Yellow River; precipitation; runoff; human activity
分类号:
P333.3
摘要:
应用Mann-Kendall趋势性检验和突变性检验法、双累积曲线法、GM（1，1）模型等方法，对黄河下游1962—2012年径流量和降水量的变化特征及规律进行了深入探讨，以期对黄河下游水资源调配，防洪减灾提供科技支撑。结果表明：降水量减少趋势不显著，突变时间为1964年，径流量减少趋势显著，突变时间为1979年。降水量和径流量变化具有明显的阶段性，降水量以1986年为界，分为丰水期、枯水期两个阶段，径流量以1979年、1985年为界，分为枯—丰—枯3个阶段，黄河目前处于枯水期。采用双累积曲线法定量分析了降水量和人类活动对径流量的影响程度。结果表明：突变时刻前，降水量和径流量同步变化，呈现正相关，突变时刻后，人类活动是影响径流量变化的主要因素，人类活动和降水量对径流量的作用比例分别为68%和32%。利用GM（1，1）模型预测了未来5年降水量和径流量的变化趋势，表明未来5年降水量和径流量将会有所增加。
Abstract:
In order to provide scientific support for the development of water resources allocation and flood control in the lower reaches of Yellow River, the characteristics and patterns of the precipitation and runoff had been discussed. The results showed that the decrease of precipitation was not significant, and the year of abrupt change was 1964 while the runoff decreased significantly, and the year of abrupt change was 1979. The changes of precipitation and runoff have obvious stage. The precipitation can be divided into two stages as the boundary of 1986, the abundant water period and the low water period. The runoff can be divided into dry-wet-dry three stages as the boundary of 1979, 1985, respectively; the Yellow River is still in the dry season, too. The effects of precipitation and human activities on runoff were quantitatively analyzed by using double cumulative curve method. The results showed that the changes of precipitation and runoff were synchronized with the change of time. The impacts of human activities and precipitation on the runoff are 68% and 32%, respectively, and the human activity is the key factor affecting the runoff in the lower reaches of Yellow River. Finally, the precipitation and runoff change trend of the lower reaches of Yellow River has been analyzed and predicted in the next five years by using the GM (1,1) model. The results show that the precipitation and runoff will slowly increase in the next five years.

参考文献/References:

[1] 张建云,王国庆,贺瑞敏,等.黄河中游水文变化趋势及其对气候变化的响应[J].水科学进展,2009,20(2):153-158.
[2] Sajikumar N, Remya R S. Impact of land cover and land use change on runoff characteristics[J]. Journal of Environmental Management, 2015,161:460-468.
[3] Khadka D, Babel M S, Shrestha S, et al. Climate change impact on glacier and snow melt and runoff in Tamakoshi basin in the Hindu Kush Himalayan(HKH)region[J]. Journal of Hydrology, 2014,511(4):49-60.
[4] 刘伟,何俊仕,陈杨.浑河流域降水与径流变化特征及同步性分析[J].水土保持研究,2016,23(1):150-154.
[5] 热孜燕,阿不都,沙拉木.1957-2009年乌鲁木齐河径流与气候变化的对应关系[J].水土保持研究,2015,22(5):289-293.
[6] 刘鑫.大凌河流域径流演变规律分析[J].水土保持研究,2015,22(2):165-170.
[7] 李夫星,陈东,汤秋鸿.黄河流域水文气象要素变化及与东亚夏季风的关系[J].水科学进展,2015,26(4):481-490.
[8] 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.
[9] 张越,付永锋,侯保俭.黄河源区径流量演变成因分析[J].人民黄河,2013,35(8):22-24.
[10] 张翠,韩美,史丽华.黄河入海径流量变化特征及其对气候变化的响应[J].人民黄河,2015,37(5):10-14.
[11] 魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,1999.
[12] 章诞武,丛振涛,倪广恒.基于中国气象资料的趋势检验方法对比分析[J].水科学进展,2013,24(4):490-496.
[13] 朱晓华,杨秀春,蔡运龙.基于灰色系统理论的旅游客源预测模型[J].经济地理,2005,25(2):232-235.
[14] 穆兴民,张秀勤,高鹏,等.双累积曲线方法理论及在水文气象领域应用中应注意的问题[J].水文,2010,30(4):47-51.
[15] 吴凯,谢贤群,刘恩民.黄河断流概况、变化规律及其预测[J].地理研究,1998,17(2):125-130.
[16] 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.
[17] 王怀柏,赵淑饶,张家军,等.1950-2010年黄河径流情势变化特点[J].人民黄河,2011,33(12):16-18.
[18] 李春晖,郑小康,杨志峰,等.黄河天然径流量变化趋势及其影响分析[J].北京师范大学学报:自然科学版,2009,45(1):80-85.
[19] 赵传晋,徐学选,陈天林,等.关川河流域土地利用变化对径流的影响[J].水土保持研究,2015,22(3):83-87.
[20] 孔岩,王红,任立良.黄河入海径流变化及影响因素[J].地理研究,2012,31(11):1981-1990.
[21] 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.

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备注/Memo

收稿日期:2015-12-06;改回日期:2016-03-18。
基金项目:国家自然科学基金面上项目（41371517）；山东省科技计划（2013GSF11706）
作者简介:潘彬(1991-),男,陕西安康人,硕士研究生,研究方向为环境演变与区域可持续发展。E-mail:849599377@qq.com
通讯作者:韩美(1963-),女,山东寿光人,教授,博士生导师,主要从事环境演变与可持续发展和流域水资源与湿地生态评价研究。E-mail:hanmei568568@126.com

更新日期/Last Update: 1900-01-01