J
John C. Wyngaard
Researcher at Pennsylvania State University
Publications - 79
Citations - 11611
John C. Wyngaard is an academic researcher from Pennsylvania State University. The author has contributed to research in topics: Planetary boundary layer & Turbulence. The author has an hindex of 39, co-authored 78 publications receiving 11117 citations. Previous affiliations of John C. Wyngaard include National Center for Atmospheric Research.
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Flux-Profile Relationships in the Atmospheric Surface Layer
TL;DR: In this article, the free constants in several interpolation formulas can be adjusted to give excellent fits to the wind and temperature gradient data, and the behavior of the gradients under neutral conditions is unusual, however, and indicates that von Karman's constant is ∼0.35, rather than 0.40 as usually assumed, and that the ratio of eddy diffusivities for heat and momentum at neutrality is ∼1.0.
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Turbulence Structure in the Convective Boundary Layer
TL;DR: In this paper, a boundary layer experiment conducted over a flat site in northwestern Minnesota is discussed, where wind and temperature fluctuations near the ground were measured with AFCRL's fast-response instrumentation on a 32 m tower with MRU probes attached at five different heights to the tethering cable of a 1300 m2 kite balloon.
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Resolution Requirements for the Simulation of Deep Moist Convection
TL;DR: In this paper, the authors provide a clear theoretical framework for the simulation of turbulent flows, and the source of the subgrid terms in the Navier-Stokes equation is clarified.
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Toward Numerical Modeling in the “Terra Incognita”
TL;DR: In this paper, the authors show that the neglected production terms can be significant and that including them in the modeled SFS flux equations yields a more general SFS model, one with a tensor rather than a scalar eddy diffusivity.
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Local Free Convection, Similarity, and the Budgets of Shear Stress and Heat Flux.
TL;DR: In this article, the conservation of Reynolds shear stress and the two components of heat flux (velocity-temperature covariance) in the homogeneous atmospheric surface layer are derived.