Coastal Model Performance Evaluation and Comparison,

Abstract

This study compares several ocean circulation models in coastal applications. The comparison is restricted to 3-D, primitive equation, free-surface models on sigma-like vertical coordinate systems. The models differ in their treatment of the barotropic flow, horizontal and vertical mixing, temporal and spatial differencing and other details. The physical accuracy and the numerical character of the models are evaluated and discussed on a variety of test problems. The coastal study processes include wave propagation, upwelling and downwelling regimes, and genesis and evolution of fronts. The study indicates that the solutions may sensibly differ from model to model. This is primarily due to: (1) different response to the calibration of the physical and numerical parameters, (2) perturbations in the dynamical balances. In general, differences in the primary features (such as front location, strength of the coastal jet) can be adjusted by adequate calibrations. Representation of the secondary features (such as internal wave propagation, temperature and salinity anomalies) may depend upon different parameterizations and numerical treatments of the same physical terms that may alter the relative importance of the dominant processes.

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Document Details

Document Type
Technical Report
Publication Date
May 01, 1997
Accession Number
ADA326300

Entities

People

  • Germana Peggion

Organizations

  • University of Southern Mississippi

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Calibration
  • Coastal Regions
  • Continental Slopes
  • Deep Water
  • Equations
  • Internal Waves
  • Ocean Currents
  • Oceans
  • Personal Information Managers
  • Regions
  • Salinity
  • Sea Surface Temperature
  • Simulations
  • Surface Temperature
  • Topography
  • Water
  • Wave Propagation

Fields of Study

  • Environmental science

Readers

  • Computational Modeling and Simulation
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers