Toward cloud resolving modeling of large-scale tropical circulations: A simple cloud microphysics parameterization

This paper discusses cloud microphysical essential for large-scale tropical circulation and the tropical climate, as well as the strategy to include them in large-scale modelsi that resolve cloud dynamics. The emphasis is on the ice microphysics, which traditional cloud models consider in a fair complex manner and where a simplified approach is desirable. An extension of the classical warm rain bulk parameterization is presented. The proposed scheme retains simplicity of the warm rain parameterization (e.g., only two classes of condensed water are considered) but introduces two important modifications for temperatures well below freezing: 1) the saturation conditions are prescribed based on saturation with respect to ice, not water; and 2) growth characteristics and terminal velocities of precipition particles are representative for ice particle, not raindrops. Numerical tests suggest that, despite its simplicity, the parametrization is able to capture essential aspects of the cloud microphsics important for the interaction between convection and large-scale evironment. As an example of the application of this parameterization, preliminary results of the two-dimensional cloud-resoulving simulation of a Walker-like circulation are presented.