Meso-American
Region (MAR)

Caption: Zoom in the ROMS grid showing a cyclonic eddy in the

Caption: SeaWiFS Colored Dissolved Matter image of
the MAR obtained from new spectral optimization algorithm developed at
The model domain is the
wider
The
horizontal resolution of the simulation is 2 km and the model has 25 vertical
layers.
No. A new simulation was started nested off-line (not run
at the same time) in the Atlantic HYCOM
World Ocean Atlas 2001 climatology
Model variables of the ocean state (temperature, salinity)
at the open ocean boundaries were relaxed to the monthly Levitus ocean climatology (Word Ocean
Atlas).
Tides were set at the boundaries by the
TPXO6
global tide model.
Monthly varying surface fluxes (wind, rain, solar, radiative heat fluxes, evaporation)
were obtained from the Comprehensive Ocean Atmosphere Dataset (COADS) climatology.
This simulation was used to understand the evolution in time and space of terrestrial runoff in waters of the Mesoamerican region using remote sensing techniques combined with river discharge model (Cherubin et al., 2008).
This simulation was also used to provide some general information on the connectivity between rivers and reef (Paris and Cherubin, 2008) and the fate of fish larvae from spawning aggregation sites.
This work was funded by the World Resources Institute (WRI), thanks to Lauretta Burke and by The Nature Conservancy (TNC) thanks to Nestor Vindevoxhel and Alejandro Arrivillaga. This study was also supported by the World Bank/GEF Coral Reef Targeted Research Program (http://www.gefcoral.org/).
Laurent Cherubin - lcherubin@rsmas.miami.edu
Claire Paris - cparis@rsmas.miami.edu
Christopher Kuchinke - kuchinke@physics.miami.edu