Covariance Function for Nearshore Wave Assimilation Systems

Abstract

Data assimilation is widely used to combine observations with dynamic models to improve model prediction. The relative weighting of the original forecast and the observations, the error covariance matrices, determine how the information is transferred from the observations to the model. It is shown that the optimization of the assimilation systems has to be driven by the data taking into account the physics of the wavefield. Whereas the temporal covariance can be modeled by a parameterized Gaussian function, for nearshore wave assimilation applications, the covariance function depends primarily on the local depth and secondly on the distance from the assimilation location. In spectral space, a skewed exponential function is suggested.

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Document Details

Document Type
Technical Report
Publication Date
Jan 30, 2018
Accession Number
AD1048549

Entities

People

  • Hans E. Ngodock
  • Jay Veeramony
  • Mark D. Orzech
  • Stylianos Flampouris

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • Energy and Power Technologies
  • Space

DTIC Thesaurus Topics

  • Atlantic Ocean
  • Data Mining
  • Data Sets
  • Earth Sciences
  • Geography
  • Grids
  • Information Science
  • Normal Distribution
  • Oceanography
  • Oceans
  • Research Facilities
  • Spatial Distribution
  • Standards
  • Statistical Algorithms
  • Statistical Analysis
  • Statistics
  • Topography

Readers

  • Atmospheric Science/Meteorology
  • Coastal Oceanography
  • Statistical inference.

Technology Areas

  • Space