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Modeling of Upwelling/Relaxation Events with the Navy Coastal Ocean Model

Authors :
NAVAL RESEARCH LAB STENNIS SPACE CENTER MS OCEANOGRAPHY DIV
Shulman, Igor
Kindle, John
Martin, Paul
deRada, Sergio
Doyle, Jim
Penta, Brad
Anderson, Stephanie
Chavez, Francisco
Paduan, Jeff
Ramp, Steve
NAVAL RESEARCH LAB STENNIS SPACE CENTER MS OCEANOGRAPHY DIV
Shulman, Igor
Kindle, John
Martin, Paul
deRada, Sergio
Doyle, Jim
Penta, Brad
Anderson, Stephanie
Chavez, Francisco
Paduan, Jeff
Ramp, Steve
Source :
DTIC
Publication Year :
2007

Abstract

The Navy Coastal Ocean Model (NCOM) is a free-surface, primitive-equation model that is under development at the Naval Research Laboratory (NRL). The NCOM-based model of the Monterey Bay area is evaluated during a series of upwelling and relaxation wind events in August-September of 2000. The model receives open boundary conditions from a regional NCOM implementation of the California Current System and surface fluxes from the Navy Coupled Ocean/ Atmosphere Mesoscale Prediction System (COAMPS(TradeMark))(COAMPS is a registered trademark of the Naval Research Laboratory). Issues investigated in this study are: NCOM-based model simulations of upwelling and relaxation events, coupling to COAMPS, use of sigma versus hybrid (sigma-z) vertical grids, and coupling with a larger-scale model on the open boundaries. The NCOM simulations were able to reproduce the observed sequence of the upwelling and relaxation events, which can be attributed, in part, to the good agreement between the observed and COAMPS winds. Comparisons with the mooring observations show that COAMPS overestimates shortwave radiation values, which makes the NCOM modeled SSTs too warm in comparison with observations. The NCOM runs forced with different resolution atmospheric forcing (3 versus 9 km) do not show significant differences in the predicted SSTs and mixed-layer depths at the mooring locations. At the same time, during the extended upwelling event, the model runs forced with 3 and 9km resolution COAMPS fields show differences in the surface circulation.<br />Published in Journal of Geophysical Research, v112, C06023, 2007. The original document contains color images.

Details

Database :
OAIster
Journal :
DTIC
Notes :
text/html, English
Publication Type :
Electronic Resource
Accession number :
edsoai.ocn831986704
Document Type :
Electronic Resource