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About Us
Three different coupled modeling systems have been developed and
improved at Goddard Space Flight Center.
The first modeling system is the improved GCE that has been developed
and improved at Goddard over last two decades. The GCE model has
recently been enhanced in its ability to simulate the impact of atmospheric
aerosol concentrations on precipitation processes and the impact of
land and ocean surface processes on convective systems in different
geographic locations. The improved GCE model has also been coupled
with a NASA TRMM microwave radiative transfer model and precipitation
radar model to simulate satellite - observed brightness temperatures
at different frequencies. This new, coupled GCE allows us to better
understand cloud processes in the Tropics as well as to improve the
precipitation retrieved from NASA satellites.
The second modeling system couples the NASA Goddard finite volume GCM
(fvGCM) with the Goddard Cumulus Ensemble model (GCE), a CRM. The use
of the fvGCM allows for global coverage and the use of the GCE allows
for the explicit simulation of cloud processes and their interactions
with radiation and surface processes. This modeling system has
been applied and its performance tested for two different climate scenarios,
El Niño (1998) and La Niña (1999). The coupled new modeling system
produces more realistic propagation and intensities of tropical rainfall
systems and intraseasonal oscillations and an improved diurnal variation
of precipitation: all are very difficult to forecast even using state-of-the-art
GCMs.
The third modeling system couples various NASA Goddard physical packages
(i.e., microphysics, radiation and land surface process) into a next
generation weather forecast model (called the Weather and Research Forecast
model or WRF.) The coupled new modeling system enables better forecasts
(or simulations) of convective systems [e.g., a mesoscale convective
system (MCS) in Oklahoma or a typhoon in the West Pacific]. WRF
has also been modified so that it can be initialized with the high-resolution
fvGCM. |