The present study is designed to provide both a method whereby the details of the nonlinear exchange process which occurs in the atmosphere may be considered in a simplified form, and also to indicate from some calculations the complexity of those exchanges.

A general numerical integration formula is presented which generates many of the commonly used one-dimensional finite-difference schemes.

During a trip to a weather station, Fly Guy and Buzz learn all about weather, discussing what controls the weather, how clouds form, and the scientists who study the Earth's climate.

In this study, the RAMS@CSU cloud-resolving mesoscale forecast model is run in a real-time configuration with a sophisticated microphysical package and multiple nested grids, in which the smallest grid has increased vertical resolution in the lower boundary layer. Using this configuration, two specific fog events are simulated in 3-D using initialization data with a horizontal resolution of 40 km.