A discrete wavelet spectrum approach for identifying non-monotonic trends in hydroclimate data
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 thei...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-01-01
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Series: | Hydrology and Earth System Sciences |
Online Access: | https://www.hydrol-earth-syst-sci.net/22/757/2018/hess-22-757-2018.pdf |
Summary: | 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 <q>warming</q> and the <q>warming
hiatus</q> 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 <q>climate</q> 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. |
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ISSN: | 1027-5606 1607-7938 |