Biblio
Filters: Author is Zilitinkevich, Sergej [Clear All Filters]
Analysis of remote sensing monitoring of the lower atmosphere temperature profile in Bergen, Norway. Russian Meteorology and Hydrology 38, (2013).
Atmospheric boundary layer over steep surface waves. Ocean Dynamics 64, (2014). Download: troitskaya_2014_atmospheric_boundary_layer_over_steep_surface_waves.pdf (2.67 MB)
Atmospheric boundary layers in storms: advanced theory and modelling applications. Advances in Geosciences 47-49 (2005).
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>
Closure schemes for stably stratified atmospheric flows without turbulence cutoff. Journal of the Atmospheric Sciences 73, (2016).
Diagnostic and prognostic equations for the depth of the stably stratified Ekman boundary layer. Quarterly J. Royal Meteorol. Soc. 25-46 (2002).
Diurnal asymmetry to the observed global warming. International Journal of Climatology (2015).
The effect of baroclinicity on the depth of neutral and stable planetary boundary layers. Quart, J. Roy. Met. Soc. 3339-3356 (2003).
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 aerodynamic roughness length and displacement height. Boundary-Layer Meteorology 129, 179-190 (2008).
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
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)
Energy-similarity a new turbulence closure model for stably stratified atmospheric boundary layers. Journal of Atmospheric Sciences (2004).
An enhanced integrated approach to knowledgeable high-resolution environmental quality assessment. Environmental Science and Policy 122, (2021).
Formation of large-scale semi-organised structures in turbulent convection. Phys. Rev. E. 66, 1-15 (2002).
Forthcoming meetings on planetary boundary layer theory, modelling and applications. Boundary-Layer Meteorology (2006).
Further comments on the equilibrium height of neutral and stable planetary boundary layers. Quarterly J. Royal Meteorol. Soc. 133, 265-271 (2007).
The Influence of large convective eddies on the surface-layer turbulence. Q.J.R. Meteorol. Soce. 1423-1456 (2006).
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>
Links between observed micrometeorological variability and land-use patterns in the highveld priority area of South Africa. Meteorology and Atmospheric Physics 118, 16 (2012). Download: Esau_etal_2012_MAPh_V118N3-4pp129-142_doi10.1007_s00703-012-0218-4.pdf (993.75 KB)
Links between observed micro-meteorological variability and land-use patterns in the highveld priority area of South Africa. Meteorology and atmospheric physics (Print) 118, (2012).
