This paper presents results of a comprehensive study of relationship between the movement of tropical cyclones and the large-scale circulation which surrounds them.
An analysis is carried out which considers the relationship of orbit mechanics to the satellite navigation problem, in particular, meteorological satellites.
A one-layer bulk boundary layer model is developed following earlier work by Randall and Moeng. The model predicts the mixed layer values of the potential temperature, mixing ratio, and u- and v-momentum. The model also predicts the depth of the boundary layer and the vertically integrated turbulence kinetic energy (TKE).
A series of studies was conducted at several arctic locations to determine the relationship between cloud condensation nuclei (CCN) and ice nuclei (IN) and the pollutant aerosol.
The erosion and subsequent mixing to the environment of the updraft of mesoscale convective clouds is examined and modeled as a mechanism for the thermal modification of the cloud environment.
The numerical study presented here has focused on baroclinic processes which contribute to tropical cyclone propagation. Two numerical models were used in this work.
