为探究变化环境下赣江流域水文极端事件季节性变化的新特征,基于赣江流域1960—2018年气象水文数据,引入Copula函数和条件概率分布建立径流与气候因素之间的概率依存关系,分析季节性径流与气候因素之间的相关性和敏感性,以及不同气候情景下水文极端事件发生的概率特征及变化。结果表明:赣江流域春季径流和降水量均呈减少趋势,其他季节呈增多趋势;对数正态分布、威布尔分布、伽玛分布和广义极值分布对气象水文要素拟合效果良好,气象要素与径流的最优Copula函数以Frank-Copula函数为主;径流与降水量、相对湿度和水汽压呈正相关,与潜在蒸散量、日照时长呈负相关,且春夏冬对降水量最敏感,秋季对日照时长最敏感;降水量从中值降至低值时,径流特枯事件发生概率平均增多16.6%,由中值增至高值时,洪水发生概率平均增多13.6%。
Abstract
The purpose of this paper is to explore the new characteristics of seasonal changes of extreme hydrological events in the Ganjiang River Basin under changing circumstances. We used hydrometeorological data from 1960 to 2018 in the basin and established the probability dependence between runoff and climatic factors using Copula function and conditional probability distribution. We analyzed the correlation and sensitivity between seasonal runoff and climatic factors, as well as the probability characteristics and changes of extreme hydrological events under different climate scenarios. Our results show that runoff and precipitation in the Ganjiang River Basin decrease in spring while increase in other seasons. Climatic hydrological elements can be well fitted by logarithimic normal distribution, Weibull distribution, gama distribution, and generalized extreme value distribution. Frank-Copula function is the optimal Copula function for meteorological elements and runoff. Runoff is positively correlated with precipitation, relative humidity, and water vapor pressure, while negatively with potential evapotranspiration and sunshine duration. Runoff is most sensitive to precipitation in spring, summer, and winter, and most sensitive to sunshine duration in autumn. When precipitation decreases from median value to low value, the probability of extremely dry runoff events increases by an average of 16.6%; when precipitation increases from median value to high value, the probability of flood occurrence increases by an average of 13.6%.
关键词
径流 /
气候因素 /
水文极端事件 /
Copula函数 /
条件概率 /
赣江
Key words
runoff /
climatic factors /
extreme hydrological event /
Copula function /
conditional probability;Ganjiang River
{{custom_sec.title}}
{{custom_sec.title}}
{{custom_sec.content}}
参考文献
[1] CHEN Q, CHEN H, ZHANG J, et al. Impacts of Climate Change and LULC Change on Runoff in the Jinsha River Basin. Journal of Geographical Sciences, 2020, 30(1): 85-102.
[2] YAN X,BAO Z,ZHANG J,et al. Quantifying Contributions of Climate Change and Local Human Activities to Runoff Decline in the Upper Reaches of the Luanhe River Basin. Journal of Hydro-environment Research,2020,28:67-74.
[3] 刘贵花, 齐述华, 朱婧瑄, 等. 气候变化和人类活动对鄱阳湖流域赣江径流影响的定量分析. 湖泊科学, 2016, 28(3): 682-690.
[4] 刘剑宇, 张 强, 邓晓宇, 等. 气候变化和人类活动对鄱阳湖流域径流过程影响的定量分析. 湖泊科学, 2016, 28(2): 432-443.
[5] 韩会明,游文荪,简鸿福, 等.赣江流域气象干旱与水文干旱特征及其概率关系.人民长江, 2021, 52(5):44-49.
[6] 李其江. 长江源径流演变及原因分析. raybet体育在线
院报, 2018, 35(8):1-5, 16.
[7] AHN K-H, MERWADE V. Quantifying the Relative Impact of Climate and Human Activities on Streamflow. Journal of Hydrology, 2014, 515: 257-266.
[8] FRANCESCO F, BARTOSZ S, ADAM K, et al. Advanced Sensitivity Analysis of the Impact of the Temporal Distribution and Intensity of Rainfall on Hydrograph Parameters in Urban Catchments. Hydrology and Earth System Sciences, 2021, 25(10): 5493-5516.
[9] SONG P, LIU W, SUN J, et al. Annual Runoff Forecasting Based on Multi-Model Information Fusion and Residual Error Correction in the Ganjiang River Basin. Water, 2020, 12(8): 2086.
[10] 游海林, 吴永明, 杜冰雪, 等. 1950—2016年赣江径流量变化特征及其影响因素分析. 水利水电技术, 2019, 50(7): 48-54.
[11] 丁倩倩, 刘友存, 焦克勤, 等. 赣江上游典型流域水沙过程对全球气候变化的响应. 长江流域资源与环境, 2020, 29(1): 174-186.
[12] 黄彬彬, 严登华, 李卿鹏. 赣江尾闾河段水环境演变规律与驱动因子分析. 人民长江, 2019, 50(增刊2): 26-29.
[13] 仝路路, 郭传波, 王 瑞, 等. 多重人类活动干扰下赣江流域水环境和鱼类资源的研究现状分析. 长江流域资源与环境, 2019, 28(12): 2879-2892.
[14]
[15] GB/T 20481—2017,气象干旱等级. 北京:中国标准出版社,2017.
[16] SKLAR M. Fonctions de Repartition a n Dimensions et Leurs Marges. Paris: Université Paris, 1959.
[17] 李艺珍,岳春芳,曹 伟. 基于滑动Copula函数的金沟河流域径流-气温关系变异诊断. raybet体育在线
院报, 2020,37(11): 33-39.
[18] 吴海鸥, 涂新军, 杜奕良, 等.基于Copula函数的鄱阳湖水系径流丰枯遭遇多维分析. 湖泊科学, 2019, 31(3): 801-813.
[19] 莫淑红, 沈 冰, 张晓伟, 等. 基于Copula函数的河川径流丰枯遭遇分析. 西北农林科技大学学报(自然科学版), 2009, 37(6): 131-136.
[20] ZHAO G, HRMANN G, FOHRER N, et al. Streamflow Trends and Climate Variability Impacts in Poyang Lake Basin, China. Water Resources Management, 2010, 24(4): 689-706.
[21] SHAO W, CHEN X, ZHOU Z, et al. Analysis of River Runoff in the Poyang Lake Basin of China: Long-Term Changes and Influencing Factors. Hydrological Sciences Journal, 2017, 62(4): 575-587.
[22] 李云良, 张 奇, 李相虎, 等.鄱阳湖流域水文效应对气候变化的响应. 长江流域资源与环境, 2013, 22(10): 1339-1347.
[23] 章 茹, 孔 萍, 蒋元勇, 等.近50年鄱阳湖流域降水时空特征及其对水文过程的驱动. 南昌大学学报(理科版), 2014, 38(3): 268-272.
[24] 蒋 艳, 周成虎, 程维明. 阿克苏河流域径流补给及径流变化特征分析. 自然资源学报, 2005(1):27-34.
[25] 魏天锋, 刘志辉, 姚俊强, 等. 呼图壁河径流过程对气候变化的响应. 干旱区资源与环境, 2015, 29(4): 102-107.
[26] 程文举,席海洋,张经天. 黑河上游径流对极端气候变化的响应研究. 高原气象,2020,39(1):120-129.
[27] 杨满根, 陈 星. 气候变化对淮河流域中上游汛期极端流量影响的SWAT模拟. 生态学报, 2017, 37(23): 8107-8116.
[28] 叶许春, 张 奇, 刘 健,等.气候变化和人类活动对鄱阳湖流域径流变化的影响研究. 冰川冻土, 2009, 31(5): 835-842.
[29] 叶许春, 刘 健, 李相虎, 等.气候和人类活动对赣江径流变化的作用分析. 河海大学学报(自然科学版), 2013, 41(3): 196-203.
[30] GUO H, HU Q, JIANG T. Annual and Seasonal Streamflow Responses to Climate and Land-Cover Changes in the Poyang Lake Basin, China. Journal of Hydrology, 2008, 355(1/2/3/4): 106-122.
[31] 涂安国, 杨 洁, 李 英, 等. 鄱阳湖流域气候变化及其对入湖径流量的影响. 水资源与水工程学报, 2015, 26(5): 35-39.
基金
江西省水利厅科技项目(201921YBKT07,202223YBKT05,202223YBKT16,202224ZDKT06)