HEAL DSpace

Implementation issues in 3D wind flow predictions over complex terrain

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dc.contributor.author Prospathopoulos, J en
dc.contributor.author Voutsinas, SG en
dc.date.accessioned 2014-03-01T01:24:30Z
dc.date.available 2014-03-01T01:24:30Z
dc.date.issued 2006 en
dc.identifier.issn 01996231 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/17291
dc.subject Flow over complex terrain en
dc.subject Micro-siting en
dc.subject Wind energy en
dc.subject.other Boundary conditions en
dc.subject.other Computational methods en
dc.subject.other Database systems en
dc.subject.other Navier Stokes equations en
dc.subject.other Reynolds number en
dc.subject.other Wind power en
dc.subject.other Complex terrain en
dc.subject.other Computational grid en
dc.subject.other Flow over complex terrain en
dc.subject.other Micro-siting en
dc.subject.other Aerodynamics en
dc.title Implementation issues in 3D wind flow predictions over complex terrain en
heal.type journalArticle en
heal.identifier.primary 10.1115/1.2346702 en
heal.identifier.secondary http://dx.doi.org/10.1115/1.2346702 en
heal.publicationDate 2006 en
heal.abstract Practical aspects concerning the use of 3D Navier-Stokes solvers as prediction tools for micro-siting of wind energy installations are considered. Micro-siting is an important issue for a successful application of wind energy in sites of complex terrain. There is a constantly increasing interest in using mean wind flow predictions based on Reynolds averaged Navier-Stokes (RANS) solvers in order to minimize the number of required field measurements. In this connection, certain numerical aspects, such as the extent of the numerical flow domain, the choice of the appropriate inflow boundary conditions, and the grid resolution, can decisively affect the quality of the predictions. In the present paper, these aspects are analyzed with reference to the Askervein hill data base of full scale measurements. The objective of the work is to provide guidelines with respect to the definition of appropriate boundary conditions and the construction of an adequate and effective computational grid when a RANS solver is implemented. In particular, it is concluded that (a) the ground roughness affects the predictions significantly, (b) the computational domain should have an extent permitting the full development of the flow before entering the region of interest, and (c) the quality of the predictions at the local altitude maxima depends on the end density in the main flow direction. Copyright © 2006 by ASME. en
heal.journalName Journal of Solar Energy Engineering, Transactions of the ASME en
dc.identifier.doi 10.1115/1.2346702 en
dc.identifier.volume 128 en
dc.identifier.issue 4 en
dc.identifier.spage 539 en
dc.identifier.epage 553 en


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