Quantifying Turbulent Shear Stress in "Real" Landscapes

Abstract

Major Goals: The wind velocity profile and the turbulent shear stresses exerted on the ground that drive aeolian sediment transport depend on the value of the aerodynamic roughness length, z0. The goal of this work was to better understand the controls on z0 values, especially in landscapes with multi-scale topography and in the presence of aeolian sediment transport. Multi-scale topography is ubiquitous in nature, yet previous empirical models for predicting z0 rely on the concept of a dominant roughness element or scale of roughness that must be assumed a priori. Aeolian transport has long been known to increase z0, but the relative importance of topography and sediment transport had not been determined under field conditions prior to this study.

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Document Details

Document Type
Technical Report
Publication Date
Jul 01, 2018
Accession Number
AD1081312

Entities

People

  • Jason P. Field
  • Jon D. Pelletier

Organizations

  • University of Arizona

Tags

Communities of Interest

  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Abstracts
  • Computational Fluid Dynamics
  • Equations
  • Field Conditions
  • Fluid Dynamics
  • Grain Size
  • High Resolution
  • Intensity
  • Landforms
  • Particle Size
  • Roughness
  • Sedimentation
  • Sediments
  • Shear Stresses
  • Topography
  • Wind
  • Wind Velocity

Fields of Study

  • Environmental science

Readers

  • Acoustical Oceanography.
  • Aerosol Science/Aerosol Physics
  • Distributed Systems and Data Platform Development