Several advective transport schemes are considered in the context of two-di
mensional scalar transport. To review the properties of these transport sch
emes, results are presented for simple advective test cases. Wide variation
in accuracy and computational cost is found. The schemes are then applied
to simulate salinity fields in South San Francisco Bay using a depth-averag
ed approach. Our evaluation of the schemes in the salinity simulation leads
to some different conclusions than those for the simple test cases. First,
testing of a stable, but nonconservative Eulerian-Lagrangian scheme does n
ot produce accurate results, showing the importance of mass conservation. S
econd, the conservative schemes that are stable in the simulation reproduce
salinity data accurately independent of the order of accuracy of each sche
me. Third, the leapfrog-central scheme was stable for the model problems bu
t not stable in the unsteady, free surface computations. Thus, for the simu
lation of salinity in a strongly dispersive setting, the most important pro
perties of a scalar advection scheme are stability and mass conservation.