首页> 外文OA文献 >Changes in Annual, Seasonal and Monthly Climate and Its Impacts on Runoff in the Hutuo River Basin, China
【2h】

Changes in Annual, Seasonal and Monthly Climate and Its Impacts on Runoff in the Hutuo River Basin, China

机译:年度,季节性和月度气候变化及其对中国河豚流域径流的影响及其影响

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Much attention has focused on the effects of precipitation (P) and temperature (T) changes on runoff (R); however, the impacts of other climatic factors need to be studied further. Moreover, the monthly and seasonal scale also need to be investigated. In this paper, we investigated the characteristics of changes in annual, seasonal, and monthly hydroclimatic variables, including R, P, T, sunshine duration (SD), relative humidity (RH), and wind speed (WS), between 1956 and 2015 in the Hutuo River basin (HTRB) using the nonparametric Mann-Kendall test, the cumulative anomaly test and the Precipitation-Runoff double cumulative curve method. Additionally, we assessed the contributions of climatic factors to changes in R in the HTRB between 1956 and 2015 using the climate elasticity method. The results indicated that significant downward trends were found for both annual and seasonal R, SD, RH, and WS. In contrast, there was a nonsignificant decrease in annual P; specifically, P significantly increased in spring and winter, but P insignificantly decreased in summer and autumn. Annual and seasonal T increased significantly. The annual R showed an abrupt change in 1979; thus, the entire study period from 1956 to 2015 was divided into two periods: the baseline period (i.e., 1956–1978) and the change period (i.e., 1979–2015). The elasticities in the climatic factors were calculated using the climate elasticity method, and the elasticity values of P, T, SD, RH, and WS were 1.84, −1.07, −2.79, 1.73, and −0.45, respectively. Increasing T was the main cause of the decline in R, and decreasing SD had a large negative contribution to the decline in R in the HTRB. This study will help researchers understand the interactions between climate change and hydrological processes at the basin scale and promote water resource management and watershed planning.
机译:很多关注都集中在沉淀(p)和温度(t)的影响(r)的影响;然而,需要进一步研究其他气候因素的影响。此外,还需要调查每月和季节性规模。在本文中,我们调查了年度,季节性和每月循环变量的变化特征,包括R,P,T,阳光持续时间(SD),相对湿度(RH)和风速(WS),在1956和2015之间在河豚河流域(HTRB)中使用非参数Mann-Kendall试验,累积异常试验和降水径流双累积曲线方法。此外,我们通过气候弹性方法评估了1956年至2015年间HTRB中r变化的气候因素的贡献。结果表明,每年和季节性r,sd,RH和WS都发现了显着的下行趋势。相比之下,每年的p减少不显着减少;具体而言,春季和冬季P显着增加,但在夏季和秋季的P显着下降。年度和季节性T显着增加。年度r在1979年表现出突然变化;因此,从1956年到2015年的整个学习期间分为两个时期:基线期间(即1956-1978)和变更期(即1979 - 2015年)。使用气候弹性方法计算气候因子中的弹性,P,T,SD,RH和Ws的弹性值分别为1.84,-1.07,-2.79,1.73和-0.45。增加T是R下降的主要原因,下降的SD对HTRB中的r的下降有很大的负面贡献。本研究将帮助研究人员了解盆地规模的气候变化与水文过程之间的相互作用,促进水资源管理和流域规划。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号