Several aspects of thermal convection in the presence of a lateral shear as
sociated with either a shear line [with velocity V(x)] or a circular vortex
[with azimuthal velocity V(r)] are considered. Parameter settings that fav
or suppression of convection near the axis of the shear Row or near the cen
ter of a cyclonic vortex are determined by looking at the structure of the
linear neutral modes at the onset of convection, or at the modes that have
the largest growth rates at highly supercritical Rayleigh numbers where the
motions are nearly inviscid. Both parallel [or axisymmetric (2D longitudin
al)] and wavy for nonaxisymmetric (3D)] disturbances are considered, althou
gh the analysis focuses on the former A weakly nonlinear amplitude equation
shows that the bifurcation is supercritical, but even in the presence of v
ertical asymmetry in the applied thermal mean gradient, there is nor a sign
ificant preference for upwelling or downwelling at the axis. Within the con
text of the linear model of convection in lateral shear, it is suggested th
at strong atmospheric vortices may suppress thermal convection in their cor
es. a mechanism possibly associated with vortex "eyes." A simple laboratory
demonstration of the main result is included.