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Observations of Flow and Turbulence in the Nocturnal Boundary Layer over a Slope
- P. Monti, H. Fernando, M. Princevac, W. Chan, T. Kowalewski, E. Pardyjak
- Environmental Science, Physics
- 1 September 2002
Measurements were conducted on an eastern slope of the Salt Lake Basin (SLB) as a part of the Vertical Transport and Mixing Experiment (VTMX) conducted in October 2000. Of interest was the nocturnal…
Similarity Scaling Over a Steep Alpine Slope
- D. Nadeau, E. Pardyjak, C. Higgins, M. Parlange
- Environmental Science, PhysicsBoundary-Layer Meteorology
- 1 June 2013
In this study, we investigate the validity of similarity scaling over a steep mountain slope (30–41$$^\circ $$). The results are based on eddy-covariance data collected during the Slope Experiment…
Understanding sprint-cycling performance: the integration of muscle power, resistance, and modeling.
- James C. Martin, Christopher J. Davidson, E. Pardyjak
- EngineeringInternational journal of sports physiology and…
- 1 March 2007
TLDR
Flux Richardson number measurements in stable atmospheric shear flows
- E. Pardyjak, P. Monti, H. Fernando
- Environmental Science, PhysicsJournal of Fluid Mechanics
- 25 May 2002
The flux Richardson number Rf (also known as the mixing efficiency) for the stably stratified atmospheric boundary layer is investigated as a function of the gradient Richardson number Rig using data…
Structure of Turbulence in Katabatic Flows Below and Above the Wind-Speed Maximum
- A. Grachev, L. Leo, S. Sabatino, H. Fernando, E. Pardyjak, C. Fairall
- Environmental Science, PhysicsBoundary-Layer Meteorology
- 10 January 2015
Measurements of small-scale turbulence made in the atmospheric boundary layer over complex terrain during the Mountain Terrain Atmospheric Modeling and Observations (MATERHORN) Program are used to…
Evening Transition Observations in Phoenix, Arizona
- A. Brazel, H. Fernando, J. Hunt, N. Selover, B. Hedquist, E. Pardyjak
- Environmental Science
- 2005
Abstract Past research has suggested that the evening transition in complex topography typically has several main features, such as (a) continued weak upslope flows persisting 3–5 h after sunset (if…
Adapting Tilt Corrections and the Governing Flow Equations for Steep, Fully Three-Dimensional, Mountainous Terrain
- H. Oldroyd, E. Pardyjak, H. Huwald, M. Parlange
- Environmental Science, PhysicsBoundary-Layer Meteorology
- 1 June 2016
In recent studies of atmospheric turbulent surface exchange in complex terrain, questions arise concerning velocity-sensor tilt corrections and the governing flow equations for coordinate systems…
Vehicle-generated fugitive dust transport: analytic models and field study
- J. Veranth, E. Pardyjak, G. Seshadri
- Environmental Science
- 1 May 2003
The MATERHORN: Unraveling the Intricacies of Mountain Weather
- H. Fernando, E. Pardyjak, T. Zsedrovits
- Environmental Science
- 22 December 2015
AbstractEmerging application areas such as air pollution in megacities, wind energy, urban security, and operation of unmanned aerial vehicles have intensified scientific and societal interest in…
Urban Fluid Mechanics: Air Circulation and Contaminant Dispersion in Cities
- H. Fernando, S. M. Lee, J. Anderson, M. Princevac, E. Pardyjak, S. Grossman‐Clarke
- Environmental Science
- 1 March 2001
Recently, many urban areas of the world have experienced rapid growth of population and industrial activity raising concerns of environmental deterioration. To meet challenges associated with such…
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