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dc.contributor.authorEidsvik, Karl Johan
dc.date.accessioned2016-04-27T09:45:57Z
dc.date.accessioned2016-04-28T07:02:45Z
dc.date.available2016-04-27T09:45:57Z
dc.date.available2016-04-28T07:02:45Z
dc.date.issued2006
dc.identifier.citationSINTEF Rapport A184, 20 p. SINTEF, 2006nb_NO
dc.identifier.isbn8214040272
dc.identifier.urihttp://hdl.handle.net/11250/2387694
dc.description-nb_NO
dc.description.abstractNumerical simulations of geophysical flows have to be done on very sparse grids. This study show that moderately stratified flows can nevertheless be predicted usefully accurate. For better grids than about  ∆x1/H~0.5 or so, recirculating domains and the characteristic wavelength of lee waves are predicted accurately while the lee wave amplitude is predicted with considerable error. The relative error of the turbulence intensity is comparable to  δ √K / √K  ~ 0.25, which is comparable to the large scale flow error and the about as accurate as any turbulence model can be. Strongly stratified flows are predicted with considerable errors even on dense grids. Oppdragsgiver Avinor ASnb_NO
dc.language.isoengnb_NO
dc.titlePrediction errors associated with sparse grid estimates of local atmospheric flowsnb_NO
dc.typeResearch reportnb_NO
dc.date.updated2016-04-27T09:45:57Z
dc.identifier.cristin1268135
dc.relation.projectStiftelsen SINTEF: 90A260nb_NO


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