Viscosity Parameterization and the Gulf Stream Separation

Abstract

Recent advances in computer architecture allow for numerical integration of state-of-the-art ocean models at basin scale with a grid resolution of 1/10 degrees or higher. At that resolution, the Gulf Stream's separation at Cape Hatteras is well stimulated, but substantial differences from observations are still observed in its path, strength, and variability. Several high resolution (1/12 degrees) North Atlantic simulations performed with the Miami Isopycnic Coordinate Ocean Model (MICOM) are discussed and the results suggest that, even with such a fine grid spacing, the modeled large scale circulation is still quite sensitive to choices in forcing and viscosity parameterization.

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Document Details

Document Type
Technical Report
Publication Date
Jan 19, 2001
Accession Number
ADP013577

Entities

People

  • Eric. P. Chassignet
  • Zulema D. Garraffo

Organizations

  • University of Miami

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Atlantic Ocean
  • Boundaries
  • Boundary Layer
  • Cape Hatteras
  • Computer Architecture
  • Dissipation
  • Dynamics
  • Fluid Dynamics
  • Grids
  • Gulf Stream
  • High Resolution
  • Mixing
  • New England
  • North Atlantic Ocean
  • Oceans
  • Simulations
  • Topography

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science/Meteorology
  • Computational Modeling and Simulation
  • Optical Physics and Photonics.

Technology Areas

  • Space