Transverse profiles of temperature and the mean velocities in the stre
amwise direction in a horizontal shear layer are presented. The variat
ion of vorticity thickness along the streamwise coordinate is examined
for the cases when both streams were at room temperature and when the
top stream was heated to 360 K. The similarity of the velocity field
is observed only near the plane of the interface of the two streams in
both cases. The vorticity thickness-velocity ratio correlation agrees
well with the data available for the isothermal shear layers. The hea
ting of one stream was not found to significantly influence the vortic
ity thickness, which is explained by the counteracting influences of v
iscosity and density changes.