Titlebook: Topics in Micrometeorology. A Festschrift for Arch Dyer; Bruce B. Hicks Book 1988 D. Reidel Publishing Company, Dordrecht, Holland 1988 Me

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The Persistence of Pollutants Downwind of a Point Source Following Termination of the Emission, region upwind of the receptor continued to contribute tracer until it was depleted by advection and vertical diffusion. These atmospheric processes are able, qualitatively, to account for the slowly decreasing air concentrations.

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The Stably Stratified Boundary Layer over the Great Plains, are in general agreement with previous modeling and observational studies for the mean and turbulence structure of the nocturnal boundary layer, with the exception that the eddy diffusivity of heat, and consequently the flux Richardson number are less than expected.

ALIBI

Arch,summarize Arch’s contributions in micrometeorology, and especially in the development of flux-gradient relationships, not in depth but in sufficient detail to give the unfamiliar reader an idea of the thoroughness of his work. Arch’s own review of the history of eddy flux measurement makes interesti

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The Streamwise Kolmogoroff Constant,omponent are related to the stress indicated by the wind profiles. The object is to determine the effective Kolmogoroff constant, .. which accords with the assumption of balance between turbulent energy production and dissipation. The mean from 60 half-hour runs made under stability conditions rangi

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Flow-Distortion Effects on Scalar Flux Measurements in the Surface Layer: Implications for Sensor Design, to crosstalk from the horizontal flux, and those due to amplification or attenuation due to flow blocking. We show that the crosstalk error can be eliminated by designing the sensor array to be vertically symmetric about its horizontal midplane. In such an array, the flow-blocking effect causes the

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Energy Budget for the Sahel Surface Layer During the ECLATS Experiment,This expedition was carried out from November 15 to December 10, 1980, during the dry period. Some data were collected by an instrumented aircraft, from which the turbulent fluxes were obtained in the boundary layer around midday; data were also collected at a surface station in order to estimate th

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The Persistence of Pollutants Downwind of a Point Source Following Termination of the Emission,than would be expected considering the duration of the release and the wind speed. A two-dimensional advection-diffusion model was used in a numerical study to investigate this effect. The results from the numerical study showed that the rate of decrease in concentrations downwind at a receptor afte