a. Too high land surface temperature particularly in the local summer
season.
b. Excessive zonality of circulation at mid and high latitudes with
weak eddy transports and low polar surface pressures.
c. Lack of skill in seasonal forecasts outside the tropics.
d. Several isolated generic deficiencies of all GCMs.
Our presentation will include major hydrologic outputs of our model higlighting
the successes and failures of the simulation. Based on the above realizations
and in preparation for second phase of AMIP, we have included cumulus downdrafts
and gravity-wave drag into the GCM.