M. Ji et al., A MULTISEASON CLIMATE FORECAST SYSTEM AT THE NATIONAL-METEOROLOGICAL-CENTER, Bulletin of the American Meteorological Society, 75(4), 1994, pp. 569-577
The Coupled Model Project was established at the National Meteorologic
al Center (NMC) in January 1991 to develop a multiseason forecast syst
em based on coupled ocean-atmosphere general circulation models. This
provided a focus to combine expertise in near real-time ocean modeling
and analyses situated in the Climate Analysis Center (CAC) with exper
tise in atmospheric modeling and data assimilation in the Development
Division. Since the inception of the project, considerable progress ha
s been made toward establishing a coupled forecast system. A T40 versi
on of NMC's operational global medium-range forecast model (MRF) has b
een modified so as to have improved response to boundary forcing from
the Tropics. In extended simulations, which are forced with observed h
istorical global sea surface temperature (SST) fields, the model repro
duces much of the observed tropical Pacific and North American rainfal
l and temperature variability. An ocean reanalysis has been performed
for the Pacific basin starting from July 1982 to present and uses a dy
namical model-based assimilation system. This also provides the ocean
initial conditions for coupled forecast experiments. The current coupl
ed forecast model consists of an active Pacific Ocean model coupled to
the T40 version of the NMC's MRF. In the future, a global ocean model
will be used to include climate information from the other ocean basi
ns. The initial experiments focused on forecasting Northern Hemisphere
winter SST anomalies in the tropical Pacific with a lead time of two
seasons. The coupled model showed considerable skill during these expe
riments. Work is currently under way to quantify the skill in predicti
ng climatic variability over North America.