A 3D hybrid (H) transport scheme has been developed that consists of the Pr
ather (P) scheme for vertical transport and a semi-lagrangian (SL) scheme f
or horizontal transport on a spherical surface. Two rests have also been de
veloped to permit evaluation of the performance of any numerical transport
scheme for flows similar to those found in the earth's atmosphere. In the f
irst test, the 2D distributions of the wind field and the 3D distribution o
f the chemical species concentration are prescribed analytically and the co
nsistent analytical expression for the species sources and sinks is determi
ned from the constituent continuity equation. The analytical expressions fo
r the winds and source and sink are then used by a numerical scheme to calc
ulate the 3D distribution of the species concentration. Comparison of the n
umerical distribution with the analytical distribution then allows evaluati
on of the performance of the numerical scheme. This test has been used to c
ompare the P, SL, and H schemes. The test shows that the SL scheme produces
errors up to 6% in species concentration. The P scheme has high accuracy (
about 1%) but requires substantial amounts of computer CPU time and memory.
The accuracy of the H scheme is higher (better than 1.6%) than that of the
SL scheme and is close to that of the P scheme. The H scheme is about nine
times faster than the P scheme but does require about three times more mem
ory than the SL scheme. In another rest, the P, H, and SL schemes are teste
d for 2D zonally averaged transport of the conservative species "cloud" by
analytically calculated wind velocities. Comparison of the results shows th
at the H scheme is superior to the SL scheme. It is concluded that the H sc
heme is a computationally efficient, accurate scheme for simulating the 3D
global transport of both conservative and nonconservative species.