Biblio
Energetics of turbulence, Ri-critical, and a new closure model for stable stratification. Atmospheric boundary layer flows in air pollution modelling , VKI LS 2008-06 (ed. by J.P.A. van Beek, J.-M. Buchlin, A. Petrosyan), von Karman Institute for Fluid Dynamics, ISBN-13 978-2-930389-85-0, D/208/0238/526, 3.1-3.7 (2008).
Turbulence energetics in stably stratified geophysical flows: Strong and weak mixing regimes. Quarterly Journal of the Royal Meteorological Society 134, 793-799 (2008).
Similarity theory and calculation of turbulent fluxes at the surface for the stably stratified atmospheric boundary layer. Boundary-Layer Meteorology 125, 193-205 (2007). Abstract
Download: fulltext-11.pdf (871.77 KB)
Turbulence closure for stably stratified flows in the atmosphere and the ocean. Ukrainian Hydrometeorological Journal (2009).at <http://www.nbuv.gov.ua/portal/natural/Uggj/index.html>
Resistance and heat transfer laws for stable and neutral boundary layers. Turbulence and Waves in Stably Stratified Atmospheric Shear Flows: Measurements, High Resolution Simulations and Numerical Prediction Challenges (2004).
Atmospheric boundary layer. NetFAM / COST TEMPUS International School and Workshop Integrated Modelling of Meteorological and Chemical Transport Processes / Impact of Chemical Weather on Numerical Weather Prediction and Climate Modelling , 7-15 July 2008, Zelenogorsk (St.Petersburg (2008).
Calculation of the height of stable boundary layers in practical applications. Boundary-layer Meteorology 389-409 (2002).at <http://www.springerlink.com/content/100245/?p=43e84a3972f3443fbe3e13aeb2578da0&pi=0>
Baroclinic Ekman Layer. Abstracts: 15th AMS Symposium on Boundary Layers and Turbulence, Wageningen, The Netherlands, 15-19 July 2002 (2002).
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
Third-order transport due to internal waves and non-local turbulence in the stably stratified surface layer. Quart. J. Roy. Met. Soc. 913-925 (2002).
Modelling the ground layer (invited presentation). 2nd ARENA Workshop on Interferometry at Dome C. European Southern Observatory (ESO) and Max Planck Institute for Plasma Physics (IPP), Garching (Munich), Germany, October 13-14, 2008. Abstract: the web site of the EU FP6 project ARENA (2008).
The effect of baroclinicity on the depth of neutrally stratified Ekman boundary layer. Abstracts: 27th EGS General Assembly, Nice, France, 21-26 April 2002 (2002).
What do we need from experiments to better model physical processes in stable boundary layers?. CD-ROM Sodankylä Seminar on Stable Boundary Layers. Sodankylä, Finland, 30-31 August 2004, Finnish Meteorological Institute. (2004).
Planetary boundary layer feedbacks in climate system and triggering global warming in the night, in winter and at high latitudes. Geography, Environment, Sustainability 1, (2009). Abstract
Scaling laws and turbulence closures for stable boundary layers. 27th EGS-AGU-EUG Joint Assembly, Nice, France, 6-11 April 2003.; CD-ROM Geophysical Research Abstracts , Volume 5, 2003. (2003).
On integral measures of the neutral, barotropic planetary boundary layers. Boundary-layer Meteorology 371-379 (2002).at <http://www.springerlink.com/content/100245/?p=43e84a3972f3443fbe3e13aeb2578da0&pi=0>
Principal comments on numerical simulation of homogeneous stably stratified turbulence. Boundary-Layer Meteorology (2010).doi:10.1007/s10546-010-9484-1 Download: fulltext-32.pdf (99.83 KB)
Energy- and flux-budget turbulence closure model for stably stratified geophysical flows. 4th International Conference on Frontiers of Nonlinear Physics (2010). Download: Nizniy_Novgorod_2010.pdf (408.12 KB)
Atmospheric boundary layers in storms: advanced theory and modelling applications. The 6th Plinius International Conference on Mediterranean Storms (Genoa Naples Palermo Palma de Mallorca Barcelona Marseille Genoa), 17-24 October 2004. (2004).
Atmospheric planetary boundary layer feedback in climate system and triggering of climate change at high latitudes. EGU General Assembly 11, (2009).
The effect of large eddies on the convective heat/mass transfer over complex terrain: Advanced theory and its validation against experimental and LES data. Croatian Meteorological Journal 20-26 (2005).
The effect of stratification on the roughness length and displacement height. ICTP Fall Colloquium on the Physics of Weather and Climate: Regional Weather Predictability and Modelling, Trieste, Italy, 29 September 10 October 2008. Abstract: the Colloquium web site (2008).
Diagnostic and prognostic equations for the depth of the stably stratified Ekman boundary layer. Quarterly J. Royal Meteorol. Soc. 25-46 (2002).
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
Download: fulltext-9.pdf (680.31 KB)
