Progress in simulating turbulence in the Meteorological Office is desc
ribed. Applications of the 'large-eddy' model include boundary layers,
gravity waves and clouds of various types. In each area there is some
evidence of good performance. The technique has considerable potentia
l for increasing our understanding of atmospheric processes and helpin
g to improve forecast model parametrizations. Validation of the model
using high-quality observations continues to be very important..