Biblio
Filtre: Forfatter er Elperin, T. [Slett Alle Filtre]
Energy- and flux-budget turbulence closure model for stably stratified geophysical flows. 4th International Conference on Frontiers of Nonlinear Physics (2010). Last ned: Nizniy_Novgorod_2010.pdf (408.12 KB)
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part II: The role of internal gravity waves. Boundary-Layer Meteorology (2009).doi:10.1007/s10546-009-9424-0
Turbulence closure for stably stratified flows in the atmosphere and the ocean. Ukrainian Hydrometeorological Journal (2009).på <http://www.nbuv.gov.ua/portal/natural/Uggj/index.html>
Turbulent diffusion and turbulent thermal diffusion of aerosols in stratified atmospheric flows. Journal of Geophysical Research 114, (2009).
Internal gravity waves in the turbulence closure problem for the stably stratified sheared flows. International Conference Mesoscale Meteorology and Air Pollution in Commemoration of the Late Professor Lev Gutman and His Outstanding Contribution to Theoretical Mesometeorology, pp. 15-17 September 2008, Odessa State Environmental University, Odessa (2008).
Turbulence energetics in stably stratified geophysical flows: Strong and weak mixing regimes. Quarterly Journal of the Royal Meteorological Society 134, 793-799 (2008).
Turbulent energetics in the stably stratified geophysical flows and the problem of critical Richardson number. International Conference Mesoscale Meteorology and Air Pollution in Commemoration of the Late Professor Lev Gutman and His Outstanding Contribution to Theoretical Mesometeorology, 15-17 September 2008, Odessa State Environmental University, Odessa, Ukra (2008).
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes. Atmospheric Boundary Layers: Nature, Theory and Applications to Environmental Modelling and Security 11-35 (2007).doi:10.1007/978-0-387-74321-9_3 Abstract
Last ned: fulltext-8.pdf (727.04 KB)
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes. Boundary-layer Meteorology 125, 167-191 (2007). Abstract
Last ned: fulltext-9.pdf (680.31 KB)
The nature and the role of semi-organised structures in the atmospheric convective boundary layers. Abstracts: 4th Annual Meeting of the European Meteorological Society, Nice, France, 26-30 September 2004 (2004).
Formation of large-scale coherent structures in turbulent convection. Abstracts: International Symposium on High Rayleigh Number Convection, Leiden, The Netherlands 10-19 June 2003 and International Symposium on Shallow Flows, Delft, the Netherlands, 16-18 June 2003 (2003).
Formation of large-scale semi-organised structures in turbulent convection. Phys. Rev. E. 66, 1-15 (2002).
Generation of Large-scale Semi-organised Structures in Sheared Turbulent Convection. Abstracts: 9th European Turbulence Conference, Southampton, UK, 2-5 July 2002 (2002).
Generation of large-scale semi-organised structures in turbulent convection. Abstracts: 27th EGS General Assembly, Nice, France, 21-26 April 2002 (2002).
