Analysis on the evolution of precipitation and Runoff characteristics in the east Pi River Basin, China

Hanjiang Nie; Zhenqian Shen; Tianling Qin; Xinfeng Gong; Yinghou Huang

doi:10.24850/j-tyca-14-02-10

Authors

Hanjiang Nie State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, China / Key Laboratory for Geographical Process Analysis & Simulation of Hubei Province, School of Urban and Environmental Sciences, Central China Normal University, Wuhan, China https://orcid.org/0000-0003-1712-1450
Zhenqian Shen Guangzhou Water Science Research Institute, Guangzhou, China
Tianling Qin State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, China
Xinfeng Gong College of Water Conservancy Engineering, Zhengzhou University, Zhengzhou, China
Yinghou Huang College of Hydrology and Water Resources, Hohai University, Nanjing, Jiangsu, China

DOI:

https://doi.org/10.24850/j-tyca-14-02-10

Keywords:

Trend and significance, abrupt change, spatiotemporal analysis, high resolution

Abstract

The natural hydrologic cycle is greatly influenced by climate change. In particular, substantial spatiotemporal variations in precipitation can occur in some mountainous areas, and thus it is very important to identify hydrological processes in watershed with high resolution. To analyze the problem above, the Mann-Kendall test, the moving T-test, Sen's slope estimator and Spearman rank correlation test combined with the spatial interpolation function of ArcGIS, are used to analyze and discuss the evolution of the spatiotemporal distribution characteristics of precipitation and Runoff in a typical small watershed of mountainous areas. The result is precipitation showed a downward trend from south to north and from high-altitude to low-altitude regions. And the difference mainly occurred in the western part of the basin. And the conclusions show the following: 1) An abrupt change in both precipitation and Runoff sequences occurred in 1991; 2) the extreme value of the precipitation trend shifted from the central region to the western region; 3) for the ratio of Runoff in the flood season to annual Runoff, the sequence showed a significant upward trend (95 % confidence level), indicating that the uneven distribution of Runoff has significantly increased since the 1960s.