Wavenumber Spectrum of Intermediate-Scale Ocean Surface Waves

Abstract

This paper presents an analysis of the wavenumber spectra of intermediate-scale waves (wavelengths between 0.02 and 6 m) under various sea-state conditions. The main result of the analysis is that the dependence of the dimensionless wave spectrum on the dimensionless wind friction velocity follows a power-law function. the coefficient and exponent of the power-law function vary systematically with the wavenumber. The wavenumber dependence of the coefficient and exponent serves as an empirical parameterization for computing the wavenumber spectra of intermediate-scale waves at different wind speeds. Calculation of the mean-square slope from the resulting wavenumber spectrum confirms that intermediate-scale waves are the dominant contributor of the ocean surface roughness. A simple formula is presented for calculating the band-pass filtered mean-square slope of the ocean surface for remote sensing applications.

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Document Details

Document Type
Technical Report
Publication Date
Jul 25, 2005
Accession Number
ADA449969

Entities

People

  • Paul Hwang

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Diffraction
  • Frequency
  • Frequency Bands
  • Frequency Shift
  • Gravity Waves
  • Ku Band
  • Law
  • Measurement
  • Military Research
  • Oceans
  • Optical Scanning
  • Remote Sensing
  • Scattering
  • Spectra
  • Surface Roughness
  • Surface Waves
  • Waves

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.