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Heat transfer / Oceanography / Convection / Turbulent Prandtl number / Partial differential equation / Boundary layer / Ekman layer / Coriolis effect / WKB approximation / Physics / Meteorology / Atmospheric sciences


KATABATIC FLOW WITH CORIOLIS EFFECT AND GRADUALLY VARYING EDDY DIFFUSIVITY IVA KAVČIČ* Department of Geophysics, Faculty of Science, University of Zagreb, Croatia BRANKO GRISOGONO Department of Geophysics, Faculty of S
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Document Date: 2007-10-12 04:57:24

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City

Breidamerkurjokull / London / Boston / San Diego / New York / /

Company

Vf / Mc Graw-Hill Inc. / Continental / Orszag S. A. / Unum / /

Continent

Antarctica / /

Country

Greenland / Croatia / Iceland / /

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Facility

stable ABL / University of Zagreb / /

IndustryTerm

approximate analytical solutions / analytical solution / analytic solutions / larger-scale weather systems / zero-order solution / analytical and numerical solutions / analytical solutions / steady state solutions / analytical tool / analytic solution / approximate solutions / numerical solutions / numerical solution / proposed analytical solutions / /

NaturalFeature

Melting Outflow Glacier / Peyto Glacier / Melting Glacier / Melting Glaciers / /

Organization

Faculty of Science / Department of Geophysics / EDDY DIFFUSIVITY IVA KAVČIČ* Department of Geophysics / Royal Netherlands Academy of Arts and Sciences / Croatian Ministry of Science / Education and Sports / Croatia BRANKO GRISOGONO Department of Geophysics / University of Zagreb / American Meteorological Society / /

Person

Weng / Danijel Belušić / EDDY DIFFUSIVITY / Van den Broeke / BRANKO GRISOGONO / Ivana Stiperski / Peter A. Taylor / Dale R. Durran / IVA KAVČIČ / Eddy Diffusivities / /

Position

King / rotating Prandtl model / Regional Climate Model / J. Atmos / analytical model / simple numerical model / numerical model / /

ProvinceOrState

New York / California / Massachusetts / /

PublishedMedium

Scientific American / /

Region

Antarctic / /

Technology

Geophysics / radiation / Heat Transfer / Simulation / T - 1 / /

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