完整後設資料紀錄
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dc.contributor.authorChang, Ching-Minen_US
dc.contributor.authorYeh, Hund-Deren_US
dc.date.accessioned2018-08-21T05:53:36Z-
dc.date.available2018-08-21T05:53:36Z-
dc.date.issued2018-04-01en_US
dc.identifier.issn0022-1694en_US
dc.identifier.urihttp://dx.doi.org/10.1016/j.jhydrol.2018.02.017en_US
dc.identifier.urihttp://hdl.handle.net/11536/144909-
dc.description.abstractThis study treats the catchment as a block box system with considering the rainfall input and runoff output being a stochastic process. The temporal rainfall-runoff relationship at the catchment scale is described by a convolution integral on a continuous time scale. Using the Fourier-Stieltjes representation approach, a frequency domain solution to the convolution integral is developed to the spectral analysis of runoff processes generated by temporal non-stationary rainfall events. It is shown that the characteristic time scale of rainfall process increases the runoff discharge variability, while the catchment mean travel time constant plays the role in reducing the variability of runoff discharge. Similar to the behavior of groundwater aquifers, catchments act as a low-pass filter in the frequency domain for the rainfall input signal. (C) 2018 Elsevier B.V. All rights reserved.en_US
dc.language.isoen_USen_US
dc.subjectSpectral analysisen_US
dc.subjectRunoff discharge variabilityen_US
dc.subjectLow-pass filtersen_US
dc.subjectTemporal non-stationary processesen_US
dc.titleSpectral analysis of temporal non-stationary rainfall-runoff processesen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.jhydrol.2018.02.017en_US
dc.identifier.journalJOURNAL OF HYDROLOGYen_US
dc.citation.volume559en_US
dc.citation.spage84en_US
dc.citation.epage88en_US
dc.contributor.department環境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.identifier.wosnumberWOS:000430902000007en_US
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