A Study of Drought and Flood Cycles in Xinyang, China, Using the Wavelet Transform and M-K Test

Author:

Gu Xinchen12ORCID,Zhang Pei2,Zhang Wenjia23,Liu Yang4,Jiang Pan5ORCID,Wang Shijie6,Lai Xiaoying6,Long Aihua23

Affiliation:

1. State Key Laboratory of Hydraulic Engineering Simulation and Safety, School of Civil Engineering, Tianjin University, Tianjin 300072, China

2. State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100044, China

3. College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832000, China

4. Chinese Research Academy of Environmental Sciences, Beijing 100012, China

5. School of Economics and Management, Southwest University of Science and Technology, Mianyang 621010, China

6. College of Management and Economics, Tianjin University, Tianjin 300072, China

Abstract

Accurately identifying and predicting droughts can provide local managers with a basis for decision-making. The Xinyang region is prone to droughts and floods, which have a large impact on local agriculture and socio-economics. This paper employs precipitation data from the Xinyang region to provide a scientific basis for drought and flood control measures in this region. The data are first treated with standardized precipitation indices (SPIs) on three-month, six-month, and nine-month time scales. Subsequently, a Morlet wavelet analysis is performed for each of the three time scales analyzed for the SPI. The results show multiple time scales of drought and flood disasters in the Xinyang region. The cycles of drought and flood disasters in the Xinyang region show different fluctuations on different SPI scales. The SPI time series reflect a strong fluctuation period of 17a for drought and flood disasters in the Xinyang region. An analysis of the variance of the wavelet coefficients showed that the first main cycle of drought and flood disasters in the Xinyang region is 7a, and the second and third sub-cycles are 4a and 13a, respectively. We conclude that floods are more frequent than droughts in Xinyang and are more likely to occur from 2017 to 2021, with a subsequent shift to droughts. Local managers should put drought prevention measures in place to deal with droughts after 2021.

Funder

National Natural Science Foundation of China

Third Xinjiang Scientific Expedition Program

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

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