On two small-scale circulation mechanisms of fine-aerosol transport in the atmospheric surface layer.

Small-scale processes are taken to mean the disturbances of the atmospheric basic background which are caused by the thermal inhomogeneity of the underlying surface and under which one can neglect the effects of both centripetal and Coriolis accelerations. Slight disturbances suggest the use of linearized hydrothermodynamic equations of a weakly compressible atmosphere. Two models are considered. In one of the models, circulation over a weakly sloping barchan is analyzed using a refined model of mountain-valley circulation (the well-known Prandtl model). The other model, which is a model of a thermal spot in a geostrophic flow, can conditionally be called 'anticonvective.' This problem is solved using the method of universal functions for parabolic equations with variable coefficients. [ABSTRACT FROM AUTHOR]