EGU23-7987
https://doi.org/10.5194/egusphere-egu23-7987
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Spatiotemporal pattern of precipitation in the Pearl River basin, China from 1951 to 2015

shirong Cai1, Kunlong Niu1, Xiaolin Mu1, and Xiankun Yang1,2
shirong Cai et al.
  • 1School of Geography and Remote Sensing, Guangzhou University, Guangzhou, China (caisr@e.gzhu.edu.cn)
  • 2Rural Non-Point Source Pollution Comprehensive Management Technology Center of Guangdong Province,Guangzhou University, Guangzhou, China (yangxk@gzhu.edu.cn)

Precipitation is one of the most important factors in hydrological cycle and climate change. Due to global climate change, the global and regional hydrological cycle has been changed significantly, and the precipitation pattern has changed, which made natural disasters happened more frequent. In this study, we taken the Pearl River Basin as a case study area and used APHRODITE dataset to investigate the spatiotemporal trend of precipitation during the period of 1951-2015 based on six extreme rainfall indices recommended by the WMO. Then, the MK test was used to verify their trend and analyze the temporal and spatial variability. The results indicated that: (1) The annual PRCPTOT in the Pearl River Basin displayed an increasing trend with an increasing rate of 0.019mm/yr. Although the number of annual rainy days was decreasing, the annual SDII exhibited an increasing trend. The annual R95P and RX1day exhibited an increasing trend, but the R95D and CWD showed a decreasing trend. The seasonal PRCPTOT increased in summer and winter, but decreased in spring and autumn. R95P and SDII displayed an increasing trend in four seasons. (2) The annual variation of PRCPTOT increased from west to east, the trend of SDII, R95P and RX1day were similar with PRCPTOT, but the high value of R95D happened in the middle and lower reaches of Xijiang River, and CWD increased from north to south. Except autumn, the seasonal spatial distribution of PRCPTOT, SDII and R95P were similar. In spring and winter, the spatial distribution of PRCPTOT, SDII and R95P increased from west to east, and from north to south in summer, indicating that the Beijiang River basin and Dongjiang River basin had a higher flood risk. (3) MK test of indices shown that the Yunnan-Guizhou Plateau was becoming drier, and the risk of extreme rainfall was increasing in the Beijiang River basin and Dongjiang River basin. The study results are valuable for future water resources management and ecological environment protection in the Pearl River Basin.

How to cite: Cai, S., Niu, K., Mu, X., and Yang, X.: Spatiotemporal pattern of precipitation in the Pearl River basin, China from 1951 to 2015, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-7987, https://doi.org/10.5194/egusphere-egu23-7987, 2023.

Supplementary materials

Supplementary material file