The correspondence ratio is developed to evaluate output from an ensemble o
f numerical weather prediction models. This measure is a simple extension o
f the threat score, or critical success index, to more than two fields and
is used to measure the divergence of the forecast fields. The ratio is comp
ared with two commonly used measures: the anomaly correlation, and the mean
square error. Results indicate that the correspondence ratio is sensitive
to the bias and, when calculated for several threshold values, can provide
information beyond that supplied by the mean-square error and anomaly corre
lation measures. The correspondence ratio is particularly useful in evaluat
ing discontinuous Acids, such as precipitation. While no one measure can pr
ovide a complete assessment of forecast success, this ratio provides useful
information that can increase our understanding of model forecast quality.