Ja. Pudykiewicz et As. Koziol, AN APPLICATION OF THE THEORY OF KINEMATICS OF MIXING TO THE STUDY OF TROPOSPHERIC DISPERSION, Atmospheric environment, 32(24), 1998, pp. 4227-4244
The most common technique used for numerical simulations of tracer mix
ing is that of the numerical solution of the advection-diffusion equat
ion with the unresolved fluxes parameterized using the similarity theo
ry. Despite correct predictions of the overall directions of transport
, models based on a numerical solution of the advection-diffusion equa
tion lack sufficient accuracy to correctly reproduce the coupling of m
ixing with small scale processes which are sensitive to the microstruc
ture of the tracer distribution. The objective of this paper is to rev
isit the basic formalism employed in numerical models used to investig
ate atmospheric tracers. The main mathematical method proposed here is
the theory of kinematics of mixing which could be applied effectively
for simulations of atmospheric transport processes. At the beginning
of the paper, we introduce simple mathematical transformations in orde
r to demonstrate how complex topological structures are created by mix
ing processes. These idealistic flow systems are essential to explain
transport properties of much more complex three-dimensional geophysica
l flows. An example of the application of the kinematics of mixing to
the analysis of tracer transport on a planetary scale is presented in
the following sections. The complex filamentary structures simulated i
n the numerical experiment are evaluated using some commonly applied s
tatistical measures in order to compare the results with the data publ
ished in the literature. The results of the experiment are also analys
ed with the help of simple conceptual models of fluid filaments. The m
icrostructure of the tracer distribution introduced in the paper is es
sential to increase our understanding of atmospheric transport and to
develop more realistic parameterizations of small-scale mixing. The pr
esented results could also be used to improve calculations of the coup
ling between microphysical processes and tracer mixing. (C) 1998 Elsev
ier Science Ltd. All rights reserved.