Analysis of Wave-Induced Errors in Turbulent Flux Measurements.

Abstract

Near surface measurements of turbulent temperature and velocity fluctuations in the ocean are obscured by relatively much larger ordered fluctuations due to surface gravity waves. Analysis of measured velocity signals in the near surface region indicated that the ratio of turbulent to wave-induced kinetic energy was consistently less than .01. To a first approximation, wave-induced fluctuations should not contribute to turbulent transport. However, small instrument errors due to misalignment, phase response, or directional response may cause significant wave-induced error in direct flux measurements. The effect on turbulent flux measurements of misalignment of the velocity sensors was examined. It was found that misalignment resulted in apparent phase shifts in the measured wave-induced signals, causing erroneous contributions to the calculated flux. For alignment errors of 3.6, the error in calculated momentum and heat fluxes could have been up to 500% and 110%, respectively. Momentum flux measurements made in deep water (with respect to the length of surface waves) were found to be less sensitive to alignment errors. The errors in this case were functions of the alignment of the flowmeter axes with the predominant wave direction.

Document Details

Document Type
Technical Report
Publication Date
Sep 01, 1975
Accession Number
ADA018297

Entities

People

  • Gerald Karl Nifontoff

Organizations

  • Naval Postgraduate School

Tags

Communities of Interest

  • Sensors

DTIC Thesaurus Topics

  • Deep Water
  • Gravity Waves
  • Heat Flux
  • Kinetic Energy
  • Measurement
  • Misalignment
  • Momentum
  • Phase Shift
  • Surface Waves
  • Waves

Fields of Study

  • Environmental science
  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Geodesy