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dc.contributor.authorChang, Ching-Minen_US
dc.contributor.authorYeh, Hund-Deren_US
dc.date.accessioned2014-12-08T15:36:40Z-
dc.date.available2014-12-08T15:36:40Z-
dc.date.issued2014-09-19en_US
dc.identifier.issn0022-1694en_US
dc.identifier.urihttp://dx.doi.org/10.1016/j.jhydrol.2014.05.037en_US
dc.identifier.urihttp://hdl.handle.net/11536/25026-
dc.description.abstractThis article presents the use of stochastic methodology for quantitative analysis of variability in stream flow discharge in response to fluctuations in lateral inflow rate, where the lateral inflow rate is considered to be the difference between rainfall and infiltration rates. In this work, we focus on the case where the temporal correlation structure of the fluctuations in the lateral inflow rate can be characterized by the statistics of random fractals. A closed-form expression quantifying the stream flow variability is therefore developed to investigate the influence of the fractal dimension of lateral inflow process and the size of time domain. It is found that the stream flow discharge variability increases with the time domain size, while the fractal dimension of lateral inflow process plays a role in the smoothness of fluctuations in stream flow discharge around the mean. (C) 2014 Elsevier B.V. All rights reserved.en_US
dc.language.isoen_USen_US
dc.subjectLateral inflow rateen_US
dc.subjectFractal dimensionen_US
dc.subjectVariance of stream flow dischargeen_US
dc.titleVariability of stream flow discharge in response to self-similar random fields of temporal fluctuations in lateral inflow rateen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.jhydrol.2014.05.037en_US
dc.identifier.journalJOURNAL OF HYDROLOGYen_US
dc.citation.volume517en_US
dc.citation.issueen_US
dc.citation.spage246en_US
dc.citation.epage249en_US
dc.contributor.department環境工程研究所zh_TW
dc.contributor.departmentInstitute of Environmental Engineeringen_US
dc.identifier.wosnumberWOS:000340977000021-
dc.citation.woscount0-
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