Research in Marine Boundary Layer Intermittency

Abstract

Wind-tunnel calibrations of turbulent-pressure sensors usually reveal deviations from ideal response. These deviations are typically reported in dimensional form (e.g., in microbars) or as a fraction of the dynamic pressure. Neither presentation gives a direct indication of the reliability of pressure statistics measured in a turbulent flow. We derive a general response equation for a turbulent-pressure probe. The coefficients in the equation are equation are obtainable from standard wind-tunnel calibration results. The form of the response equation makes it straightforward to relate the errors in measured pressure statistics of the turbulence. We demonstrate this by evaluating the reliability of measurements of some important pressure covariances, including the pressure-transport term in the turbulent kinetic energy (TKE) budget in the unstable surface layer. The preliminary finding is that the Nishiyama-Bedard sensor is capable of measuring pressure transport of TKE there to within 10-20%.

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Jan 20, 1994
Accession Number
ADA276076

Entities

People

  • John C. Wyngaard

Organizations

  • Pennsylvania State University

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Boundaries
  • Boundary Layer
  • Boundary Layer Flow
  • Calibration
  • Data Analysis
  • Data Sets
  • Dynamic Pressure
  • Equations
  • Flow
  • Large Eddy Simulation
  • Layers
  • Measurement
  • Simulations
  • Statistics
  • Turbulence
  • Turbulent Flow
  • Wind Tunnels

Fields of Study

  • Physics

Readers

  • Computational Modeling and Simulation
  • Fluid Dynamics.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers