A discrete wavelet spectrum approach for identifying non-monotonic trends in hydroclimate data

• Published in: Hydrology and earth system sciences Vol. 22; no. 1; pp. 757 - 766
• Main Authors: Sang, Yan-Fang, Sun, Fubao, Singh, Vijay P., Xie, Ping, Sun, Jian
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 26.01.2018; Copernicus Publications
• Subjects: Annual temperatures; Climate science; Discrete Wavelet Transform; Evaporation; Evaporation rate; Hydroclimate; Hydrology; Identification; Methods; Potential evaporation; Stations; Temperature; Time series; Trends; Wavelet analysis; Wavelet transforms; Weather forecasting; China
• DOI: 10.5194/hess-22-757-2018
• ISSN: 1607-7938; 1027-5606

The hydroclimatic process is changing non-monotonically and identifying its trends is a great challenge. Building on the discrete wavelet transform theory, we developed a discrete wavelet spectrum (DWS) approach for identifying non-monotonic trends in hydroclimate time series and evaluating their statistical significance. After validating the DWS approach using two typical synthetic time series, we examined annual temperature and potential evaporation over China from 1961–2013 and found that the DWS approach detected both the “warming” and the “warming hiatus” in temperature, and the reversed changes in potential evaporation. Further, the identified non-monotonic trends showed stable significance when the time series was longer than 30 years or so (i.e. the widely defined “climate” timescale). The significance of trends in potential evaporation measured at 150 stations in China, with an obvious non-monotonic trend, was underestimated and was not detected by the Mann–Kendall test. Comparatively, the DWS approach overcame the problem and detected those significant non-monotonic trends at 380 stations, which helped understand and interpret the spatiotemporal variability in the hydroclimatic process. Our results suggest that non-monotonic trends of hydroclimate time series and their significance should be carefully identified, and the DWS approach proposed has the potential for wide use in the hydrological and climate sciences.