The Intermittency of Wind‐Driven Sand Transport

Abstract

Wind‐blown sand is the main driver of dune development and dust emission from soils and is thus of fundamental importance for geomorphology, ecology, climate, and air quality. Even though sand transport is driven by nonstationary turbulent winds, and is thus inherently intermittent, current parameterizations in atmospheric models assume stationary wind and continuous transport. We draw on extensive field measurements to show that neglecting saltation intermittency causes biases in the timing and intensity of predicted fluxes. We present a simple parameterization that accounts for saltation intermittency and produces substantially improved agreement against measurements. We investigate the implications of accounting for transport intermittency in atmospheric models by analyzing 35 years of hourly wind speed data from climate simulations. We show that accounting for intermittency leads to significantly different predictions of sand mass fluxes throughout the year, with potential implications for timing and intensity of dust emission.

Document Details

Document Type
Pub Defense Publication
Publication Date
Nov 16, 2019
Source ID
10.1029/2019gl085739

Entities

People

  • Francesco Comola
  • Jasper Kok
  • Marcelo Chamecki
  • Raleigh L Martin

Organizations

  • Cold Regions Research and Engineering Laboratory
  • Swiss National Science Foundation
  • United States Army Research Laboratory
  • University of California, Los Angeles

Tags

Fields of Study

  • Environmental science

Readers

  • Coastal Oceanography
  • Fluid Mechanics and Fluid Dynamics.
  • Theoretical Analysis.