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dc.contributor.authorChang, Ching-Minen_US
dc.contributor.authorYeh, Hund-Deren_US
dc.date.accessioned2017-04-21T06:56:17Z-
dc.date.available2017-04-21T06:56:17Z-
dc.date.issued2016-08en_US
dc.identifier.issn1436-3240en_US
dc.identifier.urihttp://dx.doi.org/10.1007/s00477-015-1170-xen_US
dc.identifier.urihttp://hdl.handle.net/11536/134014-
dc.description.abstractDue to natural heterogeneity in runoff processes, the analysis of response of stream channels to the variation of lateral inflow is therefore viewed in terms of stochastic spatiotemporal processes. Based on the representation theorem, a closed-form expression is derived to describe the spectral response characteristic of stream subject to spatiotemporal fluctuations in lateral inflow. It provides a basis for evaluating the induced discharge variability in stream channels. It is found that the evolutionary power spectrum of the stream flow discharge process and therefore the variance is increased with the distance from the upstream boundary and the characteristic length scale of the lateral inflow process. Flow discharge prediction in the downstream region has a high degree of uncertainty by solving the deterministic partial differential equation.en_US
dc.language.isoen_USen_US
dc.subjectStream flow discharge variabilityen_US
dc.subjectLateral inflowen_US
dc.subjectStochastic analysisen_US
dc.titleStochastic modeling of variations in stream flow discharge induced by random spatiotemporal fluctuations in lateral inflow rateen_US
dc.identifier.doi10.1007/s00477-015-1170-xen_US
dc.identifier.journalSTOCHASTIC ENVIRONMENTAL RESEARCH AND RISK ASSESSMENTen_US
dc.citation.volume30en_US
dc.citation.issue6en_US
dc.citation.spage1635en_US
dc.citation.epage1640en_US
dc.contributor.department環境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.identifier.wosnumberWOS:000379753200006en_US
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