Turbulence resulting from Kelvin-Helmholtz instability in layers of localiz
ed stratification and shear is studied by means of direct numerical simulat
ion. Our objective is to present a comprehensive description of the turbule
nce evolution in terms of simple, conceptual pictures of shear-buoyancy int
eraction that have been developed previously based on assumptions of spatia
lly uniform stratification and shear. To this end, we examine the evolution
of various length scales that are commonly used to characterize the physic
al state of a turbulent flow. Evolving layer thicknesses and overturning sc
ales are described, as are the Ozmidov, Corrsin, and Kolmogorov scales. The
se considerations enable us to provide an enhanced understanding of the rel
ationships between uniform-gradient and localized-gradient models for shear
ed, stratified turbulence. We show that the ratio of the Ozmidov scale to t
he Thorpe scale provides a useful indicator of the age of a turbulent event
resulting from Kelvin-Helmholtz instability. (C) 2000 American Institute o
f Physics. [S1070-6631(00)02206-6].