Ê Sorbjan's most recent papers
MOST RECENT PAPERS
 
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Sorbjan Z., 1999: Similarity of Scalar Fields in the Convective Boundary Layer. Journal of the Atmospheric Sciences, 56, 7, 2212-2221.
 
Sorbjan Z.,and M.Uliasz, 1999: Large-Eddy Simulation of Air Pollution Dispersion in the Nocturnal Cloud-Topped Atmospheric Boundary Layer.
Boundary-Layer Meteorology, 91, 145-157.
 
Margolin, L. P.Smolarkiewicz and Z.Sorbjan,1999: Large-Eddy Simulations of Convective Boundary Layers Using Nonoscillatory Differencing. Physica D 133 (1999) 390-397.
 
Sorbjan Z., 2001: An evaluation of local similarity on the top of the mixed layer based on large-eddy simulations. Boundary-Layer Meteorology, 101, 183-207.
 
Sorbjan Z., 2003: Air-pollution Meteorology. Chapter 4 in: Air Quality Modeling, Theories, Methodologies, Computational Techniques, and Available Databases and Software. vol. 1, Ed. P. Zannetti.
The EnviroComp Institute.
 
Sorbjan Z., 2004: Large-eddy simulations of the baroclinic boundary layer. Boundary-Layer Meteorology, 112, 57-80.
 
Sorbjan Z., 2005: Large-eddy simulations of the atmospheric boundary layer. Chapter 5B in: Air Quality Modeling, Theories, Methodologies, Computational Techniques, and Available Databases and Software. vol. II, Ed. P. Zannetti.
The EnviroComp Institute.
 
Zurn-Birkhimer, S.M, E.M.Agee, and Sorbjan Z., 2005: Convective structure in a cold air outbrak over Lake Michigan during Lake-ICE. Journal of the Atmospheric Sciences, 62, 2414-2432. Figures 1,2,3,4,5,6,7,8,9.
 
Sorbjan Z., 2005: Statistics of scalar fields in the atmospheric boundary layer based on large-eddy simulations. Part I: Free convection. Boundary-Layer Meteorology, 116, 3, 467 - 486.
 
Sorbjan Z., 2006: Statistics of scalar fields in the atmospheric boundary layer based on large-eddy simulations. Part II: Forced convection. Boundary-Layer Meteorology,119, 1, 57-79 .
 
Sorbjan Z., 2006: Local structure of turbulence in stably-stratified boundary layers. Journal of the Atmospheric Sciences, 63, 5, 526­1537.
 
Sorbjan Z., 2006: Comments on "Flux-gradient relationship, self-correlation and intermittency in the stable boundary layer". Quarterly Journal of the Royal Meteorological Society,(April 2006, Part B, No. 617), 132, 1371-1373) (click to see the reply)
 
Sorbjan Z., 2007: Statistics of shallow convection on Mars based on large-eddy simulations. Part 1: Windless conditions. Boundary-Layer Meteorology,123,1,121-142.
 
Sorbjan Z., 2007: Statistics of shallow convection on Mars based on large-eddy simulations. Part 2: Effects of wind. Boundary-Layer Meteorology,123,1,143-157.
 
Sorbjan Z., 2007: Numerical study of daily transitions in the atmospheric boundary layer. Boundary-Layer Meteorology. Boundary-Layer Meteorology. 123, 365-383.
 
Sorbjan Z., 2008: Gradient-based similarity in the atmospheric boundary layer. Acta Geophysica, 56, 1, 220-233.
 
Sorbjan Z., 2008: Local scales of turbulence in the stable boundary layer boundary layer. Boundary-Layer Meteorology.127, 2, 261-271.
 
Sorbjan Z., 2008, Toward parameterization of the convective boundary layer in weather and climate models. Submitted to Boundary-Layer Meteorology.
 
Sorbjan Z.and B.B.Balsley, 2008: Microstructure of turbulence in the nocturnal boundary layer. Submitted to Boundary-Layer Meteorology.
 
Sorbjan Z., M. Wolff and M.D.Smith, 2008: Temperature and turbulent heat flux profiles on Mars based on Mini-TES observations.
Q. J. R. Met. Soc. 135, 644, 1776-1787.
 
Sorbjan Z., 2009: Improving non-local parameterization of the convective boundary layer. Boundar-Layer Meteorology, 130, 57-69.
 
Sorbjan Z., 2010: Gradient-based scales and similarity laws in the stable boundary layer. Q.J.Roy.Met.Soc.,136, 12-43-1254.
 
Sorbjan Z., and A.A. Grachev, 2010: An Evaluation of the Flux-Gradient Relationship in the Stable Boundary Layer. Bound-Layer Meteor., 135: 385-405.
 
Sorbjan, Z., 2012: The height correction of the gradient-based and flux-based similarity functions in the stable boundary layer. Boundary-Layer _Meteorol., 142, 21-31.
 
Sorbjan, Z., 2012: A study of the Stable Boundary Layer Based on a Single-Column. Boundary-Layer Meteorol., 142, 33-53.



 
 
 
 
 
 
 
 
 
 
 

 

 
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