The emphasis of this paper is on residue-free budgets of seasonal clim
ate forecasts. It is possible to ask the following question: given a s
easonal mean geopotential height simulation from a climate model, what
is a breakdown of that contribution from different areas of the model
physics and dynamics? In that context, the authors have examined the
maintenance of a monsoonal 500-mb ridge, the eastward shift of the Tib
etan anticyclone during an El Nino year, and the Pacific-North America
n pattern. The salient results of this study include a substantial con
tribution from the advective nonlinear dynamics toward the maintenance
(positive or negative) of the seasonal climate.