Large-eddy simulations are performed of ensembles of shallow convective clo
uds under varying shear. The scalar transports are shown to be largely unaf
fected by shear, while the momentum transport is strongly affected. The par
ametrization of the momentum fluxes is discussed. The cross-cloud pressure
gradient, commonly neglected in shallow cumulus parametrizations, is shown
to be a dominant term in the in-cloud momentum budget. The performance of t
wo possible representations of this pressure gradient, each previously prop
osed for use in deep convection parametrizations, is assessed.