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  • 1
    Monograph available for loan
    Monograph available for loan
    Prentice-Hall : Englewood Cliffs, N.J.
    Call number: AWI A7-97-0205
    Type of Medium: Monograph available for loan
    Pages: XVI, 317 Seiten , Illustrationen
    ISBN: 0138535574
    Series Statement: Prentice-Hall advanced reference series. Physical and life series
    Language: English
    Note: Contents PREFACE LIST OF SYMBOLS 1 INTRODUCTION 1.1 General Remarks 1.2 Historical Notes 2 EQUATIONS 2.1 The Continuity Equation 2.2 The Navier-Stokes Equations 2.3 The Equation of State 2.4 The First Law of Thermodynamics 2.5 Simplification of the Basic Equations 2.6 Averaging Procedures 2.7 Further Simplifications 3 STRUCTURE OF TURBULENCE 3.1 Transition and Instabilities 3.2 Statistical Description of Turbulence 3.3 Scales of Turbulent Flow 3.4 Equations of Higher Moment 3.5 Budgets of Turbulent Fluxes and Variances 3.5.1 Balance of turbulent kinetic energy 3.5.2 Heat flux balance 3.5.3 Momentum flux balance 3.5.4 Temperature and humidity variance and covariance balances 4 SIMILARITY 4.1 Dimensional Analysis and Similarity 4.2 The Monin-Obukhov Similarity Theory 4.2.1 Free convection regime 4.2.2 Neutral regime 4.2.3 Very stable regime 4.2.4 Empirical verification 4.3 The Rossby Number Similarity Theory 4.4 Local Similarity Theory 4.4.1 Stable boundary layer 4.4.2 Convective boundary layer 5 SPECTRAL ANALYSIS 5.1 General Considerations 5.2 Energy Spectra 5.3 Cross Spectra 5.4 Spatial Spectra 5.5 Spectral Curve-Fitting 5.6 Spectra and Cospectra in the Surface Layer 5.7 Spectra and Cospectra in the Mixed Layer 5.8 Spectra and Cospectra in the Stable Outer Layer 6 MODELING 6.1 General Remarks 6.2 Integral Models 6.3 First-Order Closures 6.3.1 Flow in the surface layer 6.3.2 The Ekman model 6.3.3 Effects of baroclinicity 6.3.4 Effects of thermal stability 6.3.5 Effects of slightly inclined terrain 6.3.6 The effects of nonstationarity 6.4 Nonlocal Closures 6.5 Higher-Order Closures 6.5.1 The momentum flux equation 6.5.2 The heat flux equation 6.5.3 The temperature variance equation 6.5.4 The dissipation rate equation 6.6 Large Eddy Simulation Models 7 DIFFUSION 7.1 General Considerations 7.2 The Statistical Theory of Diffusion 7.3 K-Theory Models 7.4 Gaussian Models 7.5 Laboratory and Large Eddy Simulation Experiments 7.6 Higher-Order Closure Models 7.7 Monte Carlo Methods 8 MEASUREMENTS 8.1 Introduction 8.2 Sensors 8.2.1 Wind sensors 8.2.2 Temperature sensors 8.2.3 Measurements of humidity fluctuations 8.2.4 Measurements of concentration 8.2.5 Static and dynamic characteristics of sensors 8.3 Platforms 8.3.1 Aircraft measurements 8.3.2 Balloons 8.4 Remote Ground-Based Observing Systems 8.4.1 Radars 8.4.2 Lidars 8.4.3 Sodars 8.5 Averaging of Measured Quantities 8.6 Major Field Experiments 8.6.1 The 1953 Great Plains experiment 8.6.2 The 1967 Wangara experiment 8.6.3 The 1968 Kansas experiment 8.6.4 The 1973 Minnesota experiment Epilogue APPENDIX A.1 Fourier Analysis A.2 The Sweeping Method A.3 Vector Operators REFERENCES INDEX
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 147 (1996), S. 821-834 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 22 (1982), S. 481-502 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Two types of models, describing respectively the thermal and the dynamic structure of the urban boundary layer are presented. The influence of density and height of urban buildings, urban traffic, man-made heat flux, changes of albedo and existence of an aerosol layer are tested. The models give a possibility of explaining the influence of selected factors on the atmospheric state over an urban area.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 34 (1986), S. 377-397 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A similarity theory for the atmospheric boundary layer is presented. The Monin-Obukhov similarity theory for the surface layer is a particular case of this new theory, for the case of z → 0. Universal functions which are in agreement with empirical data are obtained for the stable and convective regimes.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 35 (1986), S. 73-81 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A similarity theory presented by Sorbjan (1986) is extended by taking into consideration diffusion of passive species (e.g., specific humidity) in the atmospheric boundary layer. Theoretical similarity functions are obtained for the convective and stable-continuous regimes.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 35 (1986), S. 257-275 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The local similarity theory, presented in the recent papers of Sorbjan (1986a, b), is extended by taking into consideration spectral (u, v, w, θ) and cospectral (uw, wθ, uθ) densities in the stable-continuous boundary layer. The resulting universal expressions for spectra, cospectra and the reduced frequencies of their peaks are in agreement with empirical data from the Kansas 1968 surface-layer and Minnesota 1973 boundary-layer experiments. In addition, the universal functions for the structure parameters and the dissipation rates are also derived and shown to fit the empirical data well.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 38 (1987), S. 411-413 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 46 (1989), S. 1-11 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A further discussion of local similarity in the convective boundary layer is presented. The similarity functions are derived from budget equations for the turbulent heat flux and temperature variance. The obtained similarity curves are compared with atmospheric measurements and with large-eddy simulation results.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 47 (1989), S. 195-203 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A model for the temperature spectrum in the convective boundary layer is presented. The model is developed by using local similarity parameterization of the mixed layer. The model is compared with an idealized temperature spectrum obtained during the Minnesota experiment and exhibits behavior very similar to that observed in the atmosphere.
    Type of Medium: Electronic Resource
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