Boundary Layer Studies and Applications

A Special Issue of Boundary-Layer Meteorology in honor of Dr. Hans A. Panofsky (1917–1988)

Häftad, Engelska, 2011

AvR.E. Munn,R. E. Munn

689 kr

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Produktinformation

Utgivningsdatum2011-09-20
Mått155 x 235 x 22 mm
Vikt593 g
FormatHäftad
SpråkEngelska
Antal sidor382
FörlagSpringer
ISBN9789401069281

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Meteorologi och klimatologi inom Naturvetenskap och teknik

Hans Panofsky, 1917–1988.- Publications by Professor H. A. Panofsky in Boundary-Layer Meteorology.- The Structure of the Stably Stratified Internal Boundary Layer in Offshore Flow over the Sea.- Coherent Structures in the Very Stable Atmospheric Boundary Layer.- An Evaluation of Aircraft Flux Measurements of CO2, Water Vapor and Sensible Heat.- Spectra of Surface Wind Speed and Air Temperature over the Ocean in the Mesoscale Frequency Range in Jasin-1978.- Shapes of Annual Frequency Distributions of Wind Speed Observed on High Meteorological Masts.- Vertical Profiles of the Structure Parameter of Temperature in the Stable, Nocturnal Boundary Layer.- Time Series Analyses of Concentration and Wind Fluctuations.- The Spectral Velocity Tensor for Homogeneous Boundary-Layer Turbulence.- On the Temperature Spectrum in the Convective Boundary Layer.- Dependence of Velocity Variance on Sampling Time.- Wave Drag in the Planetary Boundary Layer over Complex Terrain.- Spatial Correlation Functions of Surface-Layer Atmospheric Turbulence in Neutral Stratification.- Internal Boundary-Layer Height Formulae — A Comparison with Atmospheric Data.- Recurrence of High Concentration Values in a Diffusing, Fluctuating Scalar Field.- Water Vapor Flux at the Sea Surface.- An Analysis Scheme for Determination of True Surface Winds at Sea from Ship Synoptic Wind and Pressure Observations.- Velocity and Temperature Spectra and Cospectra in an Unstable Suburban Atmosphere.- A Micrometeorological Investigation of Surface Exchange of O3 SO2 and NO2: A Case Study.- Effect of Finite Sampling on Atmospheric Spectra.- Observation of Organized Structure in Turbulent Flow within and above a Forest Canopy.