The results of several seasonal integrations with an atmospheric globa
l circulation model with prescribed ''perfect'' sea surface temperatur
es are presented. These experiments illustrate the results of seasonal
simulations for the years 1987 and 1988. These were a dry and a wet m
onsoon year, respectively, when compared to the average. The integrati
ons cover the period from June 1 through August 31 for both years and
were carried out at two horizontal resolutions, T42 and T106, of a glo
bal model containing two different parameterizations of surface hydrol
ogy. The seasonal differences of the motion fields, divergent circulat
ions and rainfall distributions for these respective experiments are c
ompared with the corresponding observed fields. The sensitivity of sea
sonal simulations to the initial state is explored with integrations s
tarting on two successive dates. in these experiments we diagnose diff
erences of the simulated time mean states from residue free budgets of
the complete vorticity equation.