Calculation of geopotential and temperature fields from an array of nearly continuous wind observations.

Observing systems simulation experiments were carried out to estimate the accuracy of temperatures diagnosed from the divergence equation when an array of nearly continuous (in time) wind observations is available. It was found that a useful estimate of temperature can be derived from high resolution wind observations such as those obtainable from a network of wind profiling systems. Adding the divergence and vertical motion terms to the balance equation to form the complete divergence equation reduces the errors in derived temperatures and geopotential heights. Observations on an irregularly spaced grid lead to greater errors than those on a regularly spaced grid. Moderate errors are also introduced when large scale errors in geopotential occur in the lateral boundary conditions. (from authors' abstract)