The global oceanic distributions of the transient tracers tritium, tri
tiogenic He-3, and the chlorofluorocarbon CFC-11 (CFCl3) are modeled b
y using the velocity field of the Hamburg Large Scale Geostrophic (LSG
) model. Source functions for these tracers are presented including th
e extension of the global tritium source function from 1975 to 1995. T
he tracer distributions are compared with observations. The sensitivit
y of the tritium and CFC-11 simulations tb the variation of adjustable
parameters in the source functions is determined. The adjustable sour
ce function parameters cannot be varied to simultaneously achieve both
a proper reproduction of the overall tracer inventories and the obser
ved patterns of the tracer distributions. Further improvements are onl
y possible through a change in the velocity field itself. Therefore an
thropogenic tracers indeed provide a firm reality check for model ocea
n velocity fields. The model is used to simulate the. future evolution
of transient tracer fields for different oceanic regions until the ye
ar 2050.