The Regional Oceanic Modeling System helps scientists study coastal systems in all their complexity.
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Title" West Coast Models, by Karen Green

Jim McWilliams knows there are many ways to look at an ocean. You can stand on the shoreline and judge surfing conditions at the local beach. You can fly over miles of ocean at 5,000 feet and see where the waves get rough or fly over hundreds of miles at 30,000 feet to see the effects of currents and upswells caused by wind patterns.

McWilliams helped develop a simulation and modeling code that accounts for the many scales that must be considered when studying broad ocean phenomena such as coastal circulation systems. Called the Regional Oceanic Modeling System (ROMS), the code is used by a UCLA-based research group to study the many complex events that are part of a coastal circulation system. These events include the cycling of nutrients locally and regionally and their effect on local ecologies, sediment movement and how it mixes with the waters, and localized circulation patterns caused by surface storms and resulting upswells, coastline terrain, and inflow from coastal rivers.

 

click to enlarge
Upwelling cold filaments in sea surface temperature (measured in degrees Celsius) in late summer off Northern California simulated using the Regional Oceanic Modeling System (ROMS) with 2.5 kilometer grid resolution.

McWilliams, a professor of oceanography in UCLA's department of atmospheric and oceanic sciences and Institute of Geophysics and Planetary Physics, is the principal investigator for this research project. The team also includes Nicolas Gruber, assistant professor of atmospheric and oceanic sciences, Keith Stolzenbach, professor of civil and environmental engineering, and seven other research scientists.

"We are not looking at a single question, but a whole system," says McWilliams. "We try to fit together all the various pieces to see how a regional coastal system works and how regional and global systems influence each other."

The team began studying coastal regions off the North American West Coast (NAWC) about five years ago and has been running simulations on NCSA's Origin2000 supercomputer for about three years, using several hundred thousand hours of compute time each year. Most recently, the researchers began generating simulations of circulations, ecosystems, and the geochemistry of the entire Pacific basin and then scaling down those simulations to examine conditions specific to the NAWC. The work promises to shed light on how very large-scale phenomena, such as the periodic warming of the sea surface temperature in the tropical Pacific known as El Niño Southern Oscillation, come to be. It will also show how more localized currents and conditions influence each other.

According to McWilliams, the work tends to be done in pieces. A simulation might model carbon cycles and show their relationship to phytoplankton blooms, for example. Another might illustrate sediment circulation. The team looks at these pieces of the whole and puts them together to understand the bigger picture. The goal is to create an accurate model of the NAWC regional system using both ROMS and data from sensors and sampling.

 

Access Online | Posted 3-25-2003