A time integration scheme based on semi-Lagrangian advection and
Laplace transform adjustment has been implemented in a baroclinic
primitive equation model. The semi-Lagrangian scheme makes it
possible to use large time steps. However, errors arising from the
semi-implicit scheme increase with the time step size. In contrast,
the errors using the Laplace transform adjustment remain relatively
small for typical time steps used with semi-Lagrangian advection.
Numerical experiments confirm the superior performance of the Laplace
transform scheme relative to the semi-implicit reference model. The algorithmic
complexity of the scheme is comparable to the reference model,
making it computationally competitive, and indicating its potential
for integrating weather and climate prediction models.