The climate of the eastern Pacific plays an important role in the
El Niño-Southern Oscillation and thus in global climate. This region,
though, has been notoriously difficult to simulate realistically in
climate models. IPRC researchers have developed a model, the iROAM
(IPRC regional ocean-atmosphere model) that couples the IPRC regional
atmospheric model (IPRC Climate, Vol. 2, No. 2)
with the GFDL Modular Ocean Model. The ocean model covers the entire
tropical Pacific, and the atmospheric model covers the eastern half of
the Pacific as well as Central America and most of South America.
In collaboration with the Kyousei-7 Project at the Frontier Research
Center for Global Change (Frontier), the model has been adapted to run
on Japan's Earth Simulator. The iROAM has successfully captured the
salient features of eastern Pacific climate that have been so difficult
to simulate, including the northward displaced intertropical convergence
zone (ITCZ) and the equatorial annual cycle.
As in observations, the model ITCZ stays north of the equator most of the
year except for a brief period in March and April when equatorial sea
surface temperatures reach their annual maximum. IPRC Climate, Vol. 6, No. 1