Conservative high-resolution, or shock-capturing, methods have become widel
y used for modeling transport equations described by conservation laws. In
many geoscience applications, the transport equation is coupled to a conser
vation or continuity equation for a velocity field. Depending on how the ve
locity is approximated, the continuity equation may or may not be satisfied
, either locally or globally. In this paper, we discuss the effect this has
on a typical high resolution scheme, and propose a correction which accoun
ts for the fact that the velocity may be nonconservative. We present severa
l numerical examples and prove stability bounds and an a priori error estim
ate for the corrected method.