The Predictability of Near-Coastal Currents Using a Baroclinic Unstructured Grid Model

Abstract

A coastal forecast system consisting of a baroclinic unstructured grid model one-way coupled to meteorological and regional models is applied at the mouth of Chesapeake Bay. The sources of error in two-day forecasts of three-dimensional currents, produced from 4 to 14 June 2010, are analyzed by comparison to real-time observations. Of the regional model initialization and boundary forcing, the applied tides and wind forcing, the winds are the single largest contributor to errors in the predicted currents. Higher resolution winds (3 km) do reduce the error and are necessary to appropriately capture diurnal tidal interactions. However, the 3 km resolution meteorological model is still to coarse to represent winds subject to strong interaction with the shoreline. Results also confirm that wind resolution plays a large role in establishing realistic thermal and density structures in upwelling prone regions in both the regional model and consequently currents predicted by the coastal model.

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Document Details

Document Type
Technical Report
Publication Date
Dec 28, 2011
Accession Number
ADA563407

Entities

People

  • Cheryl A. Blain
  • Kendra M. Dresback
  • Mustafa K. Cambazoglu
  • Randall L. Kolar
  • Robert S. Linzell

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Bays
  • Boundaries
  • Boundary Layer
  • Chesapeake Bay
  • Civil Engineering
  • Computational Science
  • Coordinate Systems
  • Grids
  • High Resolution
  • Measurement
  • Naval Shore Facilities
  • Oceanography
  • Oceans
  • Surface Temperature
  • Terrain
  • Three Dimensional
  • Topography

Fields of Study

  • Environmental science

Readers

  • Coastal and Marine Engineering/Sediment Transport/Hydraulic Engineering
  • Finite Element Method (FEM) for solving Partial Differential Equations (PDEs)
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers