[1]WANG Shaoye,NI Yongxin,PENG Hua,et al.Temporal and Spatial Variation Characteristics and Influencing Factors of Water Yield Coefficient in the Growth Season of Yanhe River Basin in the Past 20 Years[J].Research of Soil and Water Conservation,2023,30(03):423-429.[doi:10.13869/j.cnki.rswc.2023.03.015]
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Temporal and Spatial Variation Characteristics and Influencing Factors of Water Yield Coefficient in the Growth Season of Yanhe River Basin in the Past 20 Years

References:
[1] 房平,马云,申杰,等.延河流域水生态环境存在问题及对策[J].人民黄河,2022,44(1):80-82,88.
[2] Shi C, Yuan S, Shi C, et al. Estimating the effect of precipitation and vegetation on water yield in northern China[J]. Polish Journal of Environmental Studies, 2018,27(1):305-311.
[3] 许科研,方一平,鲍文.长江黄河源区降水量变化对水资源的影响[J].人民黄河,2010,32(5):21-22.
[4] Shi X, Qin T, Yan D, et al. Analysis of the Changes in the Water Yield Coefficient over the Past 50 Years in the Huang-Huai-Hai River Basin, China[J]. Advances in Meteorology, 2018,doi.org/10.1155/2018/6302853.
[5] Lu H, Yan Y, Zhu J, et al. Spatiotemporal water yield variations and influencing factors in the Lhasa River Basin, Tibetan Plateau[J]. Water, 2020,12(5):1498.
[6] 罗宇,尹殿胜,穆兴民,等.延河流域实际蒸散发时空特征及影响因素分析[J].中国水土保持科学,2021,19(4):51-59.
[7] 陈天林,徐学选,张北赢,等.黄土丘陵区刺槐生长季生态需水研究[J].水土保持通报,2008,28(2):54-57.
[8] 刘露,朱得胜,夏帆,等.延河流域土地利用变化特征分析[J].地理空间信息,2021,19(5):38-41.
[9] 顾朝军,穆兴民,孙文义,等.极端暴雨洪水及侵蚀产沙对延河流域植被恢复响应的比较研究[J].自然资源学报,2017,32(10):1755-1767.
[10] 刘强,穆兴民,赵广举,等.延河流域水沙变化及其对降水和土地利用变化的响应[J].干旱区资源与环境,2021,35(7):129-135.
[11] 陈中平,徐强. Mann-Kendall检验法分析降水量时程变化特征[J].科技通报,2016,32(6):47-50.
[12] 李鸿雁,原若溪,王小军,等.吉林省泥石流易发区的降雨特征分析[J].自然资源学报,2016,31(7):1222-1230.
[13] 李燕,张凯瑞.黄土高原不同植被覆盖/土地利用等对蒸散发量的影响[J].人民黄河,2021,43(12):68-73.
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