Mean characteristics of the rainfall forecasts produced by the global data
analysis-forecast system of India are examined for the summer monsoons of 1
993-1996. Further, daily rainfall forecasts (accumulated for 24 h) extendin
g from day 1 to day 5 are utilised to compute monthly/seasonal mean forecas
t fields to study their consistency and reliability. Global patterns of rai
nfall forecasts are also compared with the large scale rainfall climatologi
cal fields. In addition, observed rainfall distributions over India are use
d for regional verification of the medium range rainfall forecasts.
The forecasts appear to reproduce most of the large scale features of rainf
all, except the sharp gradients over the Deccan plateau (leeside of the Wes
tern Ghats-west coast mountains over the south of Peninsular India) and the
Gangetic plains over the north of India. Further, it is found that the for
ecast model has a characteristic tendency to reduce the quantum of rainfall
over northwest India and the north Indian plains to the south of the Himal
ayas. In addition, in this study, certain aspects of the year-to-year varia
bility of the predicted rainfall fields and their associated characteristic
s are examined along with the other systematic errors of the model. It is f
ound that in this case, the sources of systematic errors could at least par
tially be eliminated, the rainfall forecasts up to day 3 or so can become a
very useful product of interest. Copyright (C) 1999 Royal Meteorological S
ociety.