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WIND CHARACTERISTICS OF MESQUITE STREETS IN THE NORTHERN CHIHUAHUAN DESERT, NEW MEXICO, USA
Citation:
GILLETTE, D., J. E. HERRICK, AND G. A. HERBERT. WIND CHARACTERISTICS OF MESQUITE STREETS IN THE NORTHERN CHIHUAHUAN DESERT, NEW MEXICO, USA. ENVIRONMENTAL FLUID MECHANICS. Springer, New York, NY, 6(3):241-275, (2006).
Impact/Purpose:
The objectives of this task include: (1) to continuously evaluate and analyze the forecast results to provide diagnostic information on model performance and inadequacies to guide further evolution and refinements to the CMAQ model, and (2) extending the utility of the daily air quality forecast model data being produced by NOAA's National Weather Service (NWS) as part of a NOAA/EPA collaboration in air quality forecasting, to EPA mission-oriented activities. These objectives include developing and maintaining a long-term database of air quality modeling results (ozone and PM2.5), performing periodic analysis and assessments using the data, and making the air quality database available and accessible to States, Regions, RPO's and others to use as input data for regional/local scale air quality modeling for policy/regulatory purposes.
Description:
The most active areas for sand movement in the mesquite-dominated ecosystems in the northern part of the Chihuahuan Desert are elongated bare soil patches referred to as "streets." Wind properties were measured at two flat mesquite sites having highly similar sandy textures but very different configurations of mesquite. Wind direction, friction velocity, aerodynamic roughness height and zero plane displacement height were estimated for 15-m tower and 3-m mast data. These aerodynamic data allowed us to distinguish five categories with differing potentials for sediment transport. Sediment transport for the five categories varied from unrestricted, free transport to virtually no transport caused by vegetation protection from wind forces. In addition, "steering" of winds below the level of the tops of mesquite bushes and coppice dunes allowed longer parallel wind durations and increased wind erosion for streets that aligned roughly SW-NE.