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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Physical geography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (252 pages)
    Edition: 1st ed.
    ISBN: 9783319436043
    Series Statement: Physics of Earth and Space Environments Series
    DDC: 551.5
    Language: English
    Note: Intro -- Preface -- Contents -- Acronyms and Symbols -- 1 Introduction -- 1.1 The Basic Definition of the Planetary Boundary Layer -- 1.2 A Few Words About Turbulence -- 1.3 The Structure and Evolution of the PBL -- 1.3.1 Local Equilibrium -- 1.3.2 Heterogeneities and Unsteadiness -- 1.3.3 The Boundary Layer Depth -- 1.4 The Transport Problem and the Turbulent Dispersion -- 1.5 Observations -- 1.6 Numerical Experiments and Simulations -- Appendix -- SGS 2002 -- CABAUW -- CCT -- SABLES98 -- ARTIST-CBL -- Other Relevant Data Sets -- References -- 2 A Summary of Mathematics and Physics for PBL -- 2.1 Eulerian and Lagrangian Description -- 2.2 The Equations for Velocity and Passive Scalars -- 2.2.1 The Navier-Stokes Equations (NSE) in a Rotating Reference Frame -- 2.2.2 The Hydrostatic Pressure and the PBL Form of NSE -- 2.2.3 The Continuity Equation -- 2.2.4 The Equation for a Passive Scalar -- 2.2.5 A Little Thermodynamics -- 2.2.5.1 The Adiabatic Gradient of Temperature -- 2.2.5.2 The Potential Temperature -- 2.2.5.3 The Virtual Temperature -- 2.2.6 The Equations for the Temperature and for the Potential Temperature -- 2.2.7 The Nondimensional Form of the Equations -- 2.3 Stochastic Variables -- 2.3.1 Probability Density Function and Moments -- 2.3.2 Averaging -- 2.3.2.1 Ensemble Average -- 2.3.2.2 Time Average -- 2.3.2.3 Volume Average -- 2.3.3 Covariances and Spectra -- 2.3.3.1 Eulerian Covariances -- 2.3.3.2 Lagrangian Covariances -- 2.3.3.3 Integral Scales -- 2.3.3.4 The `Frozen Turbulence' Approximation -- 2.3.3.5 Averaging Time and Correlation Time -- 2.3.3.6 Cospectra, Power Spectra -- 2.3.3.7 Average and Spectra -- 2.3.3.8 A Remark About Notation -- 2.4 Reynolds Averaged Equations -- 2.4.1 The Equations for the First-Order Moments -- 2.4.1.1 The Geostrophic Wind -- 2.4.2 The Equations for the Fluctuations. , 2.4.3 The Equations for the Second-Order Moments of Velocity -- 2.4.3.1 The Equation for the Mean Turbulent Kinetic Energy (TKE) -- 2.4.4 The Equation for the Temperature Variance -- 2.4.5 The Equations for the Heat Fluxes -- 2.4.6 The Interpretation of the Fluctuation Covariances and the Eddy Diffusion Model -- 2.5 Universal Features of Shear-Dominated Turbulence -- 2.5.1 Velocity Covariances and Spectra -- 2.5.1.1 Eulerian Description -- 2.5.1.2 A Model Spectrum, from from Olesen et al.(1984) -- 2.5.1.3 From k to ω: Spectra in the Frozen Turbulence Approximation -- 2.5.1.4 Lagrangian Description -- 2.5.1.5 The Eulerian-to-Lagrangian Time Scale Ratio -- 2.5.2 The Spectra of the Passive Tracer Variances -- 2.5.3 Some Consequences of Isotropy -- 2.5.4 Final Remarks -- Exercises -- References -- 3 The Basic Paradigm: Horizontal Homogeneity Over Flat Terrain -- 3.1 The Governing Equations -- 3.2 Inner and Outer Scaling from the Wind Profile -- 3.3 Similarity, Obukhov Length and Beyond -- 3.4 The Surface Layer in Neutral and Unstable Conditions -- 3.4.1 The Quasi-Neutral Conditions and the Mean Wind Profile -- 3.4.2 Unstable Conditions -- 3.4.2.1 The Mean Velocity Profile -- 3.4.2.2 The Mean Temperature Profile -- 3.4.2.3 Richardson Numbers, Eddy Diffusion Coefficientsand the Turbulent Prandtl Number -- 3.4.3 The Higher-Order Moments of the Velocity Components and of the Temperature Fluctuations -- 3.4.3.1 The Variances of the Velocity Components -- 3.4.3.2 The Third- and Fourth-Order Moments of the Velocity Components -- 3.4.3.3 The Share of the TKE Among Components -- 3.4.3.4 The Variance of the Temperature Fluctuations and the Horizontal Heat Flux -- 3.4.3.5 The Temperature Skewness -- 3.4.3.6 The Dissipation of the TKE -- 3.5 The Outer Region in Neutral Conditions -- 3.5.1 The Mean Velocity in the Ekman Layer. , 3.5.2 Truly-Neutral and Conventionally-Neutral Boundary Layers -- 3.5.3 Resistance Laws -- 3.6 Some Features of the Convective Boundary Layer -- 3.6.1 Second- and Third-Order Moments of Fluctuations -- 3.6.2 The Morning Growth of the CBL -- 3.6.2.1 The `Encroachment' Model -- 3.6.2.2 The Effects of Surface Friction and of the Entrainment at the Top -- 3.6.3 The Day-Night Transition and the Residual Layer (RL) -- 3.7 Stable Boundary Layers -- 3.7.1 Local Similarity -- 3.7.1.1 The Mean Velocity Profile -- 3.7.1.2 The Mean Temperature Profile -- 3.7.1.3 The Eddy Diffusion Coefficients and the Richardson Numbers -- 3.7.2 The Second-Order Moments -- 3.7.3 The Nieuwstadt (1984) Model -- 3.7.4 The Neutral and Stable Boundary Layer Depth -- 3.8 Some Remarks About the Spectra -- Exercises -- References -- 4 Horizontal Heterogeneities -- 4.1 Explicit Treatment vs. Parameterization -- 4.1.1 A Criterion for Horizontal Homogeneity -- 4.2 Internal Boundary Layers -- 4.2.1 Roughness Length Changes -- 4.2.2 The Thermal IBL at the Sea-Land Transition -- 4.3 The Boundary Layer Over Hills and Valleys -- 4.3.1 The Linearized Equations -- 4.3.2 The Inner and Outer Layer Concept in the Neutral Flow -- 4.3.3 The Outer Layer and the Stratification Effects -- 4.3.3.1 The Linearized Equation for the Vertical Velocity -- 4.3.3.2 A Simple Solution for the Outer Layer -- 4.3.4 A Discussion About the Inner Layer -- 4.3.5 The Turbulent Wake and the Separation -- 4.3.6 Spectra Modifications -- 4.4 Subgrid Effects of the Heterogeneous Surface Features -- 4.4.1 Distributions of Roughness Elements on a Flat Surface -- 4.4.2 The Effective Roughness of Topography -- 4.5 Low Wind, Small Vertical Fluxes -- 4.6 Canopy Flow and the Urban PBL -- 4.6.1 Some Scales and the Drag Due to the Buildings -- 4.6.1.1 Averaging the Velocity into the Canopy -- 4.6.1.2 The Canopy Drag. , 4.6.2 The Flow Above the Canopy -- 4.6.3 The Average Flow in a Volume with an Array of Solid Obstacles: The Urban Canopy Layer -- 4.6.3.1 Some Observations of the Flow in an Array of Obstacles -- 4.6.3.2 A Model for Mean Wind and Momentum Flux -- 4.6.4 Heterogeneous Urban Canopy -- 4.6.4.1 The Flow Around Buildings and the Urban Canyons -- Exercises -- References -- 5 Turbulent Dispersion -- 5.1 The Transport Problem for Fluid Parcels -- 5.1.1 Probability Density Functions, Concentration and Well Mixed Condition (WMC) -- 5.2 Absolute Dispersion of Tracer Parcels -- 5.2.1 Steady Homogeneous Conditions:Taylor(1921) -- 5.2.1.1 Dij vs. Kτ -- 5.2.2 Extension to Inhomogeneous Conditions -- 5.2.2.1 The Mean Shear Case -- 5.2.2.2 Effect of the Inhomogeneity of the Second-Order Moments on the Ballistic Regime -- 5.2.2.3 A PBL Problem: The Effect of a Wall -- 5.3 Two-Parcel Dispersion -- 5.3.1 The Dispersion in the Inertial Subrange -- 5.3.2 The Diffusive Phase -- 5.4 Meandering -- 5.5 Observations of Dispersion -- 5.5.1 Mikkelsen et al. (1987): Horizontal Meandering and Relative Dispersion in the Surface Layer -- 5.5.2 Vertical and Lateral Dispersion in a Laboratory CBL -- 5.6 The Stochastic Approach to the Absolute Dispersion of Tracer Parcels -- 5.6.1 The Link Between the Eulerian and LagrangianDescriptions -- 5.6.2 The Model with Uncorrelated Velocities: N=3 -- 5.6.2.1 A Simple Example -- 5.6.2.2 The Extension to Compressible Flows -- 5.6.3 The Model with Uncorrelated Accelerations: N=6 -- 5.6.3.1 The Derivation of the LE Terms -- 5.6.3.2 Discussion of the Model with Gaussian fE -- 5.6.3.3 A Different Model Formulation -- 5.6.3.4 Comments to the N=6 Model -- 5.7 Dispersion of Inertial Particles -- 5.7.1 The Parameterization of the Integral Time Scales for Particles -- Exercises -- References -- 6 Numerical Modeling of Turbulence for PBL Flows. , 6.1 Introduction -- 6.2 Closures for the Reynolds-Averaged Equations -- 6.2.1 The Eddy Diffusion Model for the RANS Equations -- 6.2.1.1 Eddy Diffusion Coefficient Based on the Mean Shear -- 6.2.1.2 A Clue Concerning Heterogeneity -- 6.2.1.3 Eddy Diffusion Coefficient Based on TKE -- 6.2.2 The Closure for the Second-Order Moment Equations -- 6.2.2.1 The Third-Order Term Closure -- 6.2.2.2 The Dissipation Terms and the Small Scale Isotropy -- 6.2.2.3 The Boundary Layer Approximation -- 6.2.2.4 The Lower Boundary Condition -- 6.2.2.5 Stability Corrections -- 6.2.3 TKE and TPE Based Models -- 6.2.4 The CBL and the Problem of Non-diffusive Behaviour (Counter-Gradient Fluxes) -- 6.3 Large Eddy Simulations -- 6.3.1 Filtered Equations -- 6.3.1.1 Some Definitions -- 6.3.1.2 The Continuity Equation -- 6.3.1.3 The Filtered Momentum Equation -- 6.3.1.4 The Equations for the Kinetic Energy of the Filtered Velocity and for the Residual Kinetic Energy -- 6.3.2 Closure of the Filtered Equations -- 6.3.2.1 The Smagorinsky (1963) Model -- 6.3.2.2 The Germano Dynamic Model for the Subgrid Scale Motion -- 6.3.3 The Transition from RANS to LES -- 6.4 Numerical Simulations of PBL Problems -- Exercises -- References -- Solutions -- Exercises of Chap.2 -- Exercises of Chap.3 -- Exercises of Chap.4 -- Exercises of Chap.5 -- Exercises of Chap.6 -- References -- Index.
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  • 2
    Online Resource
    Online Resource
    [Cham] : Springer
    Keywords: Meteorology ; Atmospheric sciences ; Fluids ; Geophysics ; Environmental sciences ; Physics ; Physics ; Meteorology ; Atmospheric sciences ; Fluids ; Geophysics ; Environmental sciences
    Description / Table of Contents: This book offers a comprehensive review of our current understanding of the planetary boundary layer, particularly the turbulent exchanges of momentum, heat and passive scalars between the surface of the Earth and the atmosphere. It presents and discusses the observations and the theory of the turbulent boundary layer, both for homogeneous and more realistic heterogeneous surface conditions, as well as the dispersion of tracers. Lastly it addresses the main problems arising due to turbulence in weather, climate and atmospheric composition numerical models. Written for postgraduate and advanced undergraduate-level students and atmospheric researchers, it is also of interest to anyone wanting to understand the findings and obtain an update on problems that have yet to be solved
    Type of Medium: Online Resource
    Pages: Online-Ressource (XVI, 241 p. 72 illus., 62 illus. in color, online resource)
    ISBN: 9783319436043
    Series Statement: Physics of Earth and Space Environments
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 25 (1976), S. 47-54 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Die von einigen Autoren in verschiedenen Höhen bestimmten Größenspektra der stratosphärischen Teilchen sind mit der modifizierten Gamma-Verteilungsfunktion analysiert worden, um entsprechende Modelle für die Größenverteilung zu finden. Die Ergebnisse zeigen einen Zusammenhang zwischen der Schiefea 3 und dem Radiusr c der in der Größenverteilung am häufigsten auftretenden Teilchen an. Dieser Zusammenhang wird durch die Gleichunga 3=−1.584–1.291 lnr c dargestellt und gibt die Möglichkeit, Größenverteilungsmodelle für die verschiedenen Höhenbereiche sowohl für die Aitken-Kerne als auch für die großen Sulfatteilchen, die in den stratosphärischen Schichten suspendiert sind, zu bestimmen.
    Notes: Summary Size spectra of stratospheric particles sampled by some authors at different altitudes have been analyzed in terms of the modified gamma distribution function in order to derive appropriate size distribution models. The examination of the results suggests a relationship between the skewnessa 3 and the mode radiusr c of the size distribution which can be expressed by the equationa 3=−1.584–1.291 lnr c . Such a relationship gives the opportunity to determine for the various altitudes size distribution models concerning both the Aitken nuclei and the large sulfate particles suspended in the stratospheric layers.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Based on the average variability of the skewness with respect to the droplet mode radius, a wide set of mean size-distribution models is presented in terms of the modified gamma function for fog and stratified cloud droplets. These models appear appropriate for giving reliable size-distribution curves relative to the various formation stages of the droplet population both in fogs and in stratus and stratocumulus clouds. The corresponding volume extinction coefficient has been computed at various wavelengths from 0.4 to 17 μm using Van de Hulst's (1957) approximation multiplied by Deirmendjian's (1960) correction factors. This set of theoretical extinction data has been compared with experimental extinction measurements performed in atmospheres characterized by a marked thermal inversion for describing the evolutionary features of the water droplet size distribution within the whole ground layer.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 120 (1982), S. 286-325 
    ISSN: 1420-9136
    Keywords: Scavenging of aerosol particles ; Wet removal of aerosol particles ; Aerosol particles scavenging of by drops and ice crystals
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The removal of particulate matter from the atmosphere has been examined in the light of the physical mechanisms involved, with a review of the theoretical and experimental results available in the literature. While the wet and dry removal are usually separately discussed, it has been decided to give evidence of the fundamental mechanisms which are active in both processes. A number of them, such as the inertial impaction, the phoretic and electrostatic collection, can be expressed through the equation of motion of the individual particle. Other mechanisms, such as Brownian and turbulent deposition, and incorporation by nucleation, require a description in terms of the behaviour of a population of particles. Finally, the problem of the superposition of the different mechanisms in the actual removal processes has been faced. The available experimental results have been consistently presented and compared when possible, in the same sequence, for each physical mechanism discussed in the presentation.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 14 (1978), S. 331-340 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Measurements of vertical profiles of pollen concentration from local and remote sources have been made during convective conditions with balloon-mounted rotating impaction samplers. The vertical profiles of local particles appear to be usually characterized by a decrease in the ground layer and by almost constant values aloft. A minimum often occurs at levels between 100 and 200 m. The concentration profiles of pollen from remote sources present a peak at heights of some hundred meters. By comparing the observed profiles with some published models of transport, it appears that: (i) because of differing eddy scales, turbulent transport affects the settling of pollen differently close to the ground than aloft; and (ii) turbulent anisotropies related to the dynamic and thermal structure of the atmosphere may affect the vertical distribution of particulate matter in the boundary layer.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 14 (1978), S. 585-595 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A wide set of published mass and heat transfer data is reviewed in terms of the stochastic renewal theory. A simple model is then proposed describing the transfer in terms of the fluid bulk properties. Two expressions are presented and they enable us to evaluate the bulk transfer velocity as a function of the turbulence of the flow for smooth and fully-rough surfaces in large ranges of Schmidt (or Prandtl) and Reynolds numbers. The transfer over transitional surfaces can also be evaluated by using a simple criterion for the choice of the right expression. The proposed relationships agree satisfactorily with data from laboratory and atmospheric measurements, for both solid and liquid surfaces.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 32 (1985), S. 257-279 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The problem of two-dimensional, non-rotating, stably stratified fluid flow over a pair of ridges has been investigated by means of a linearized laminar boundary-layer theory and laboratory visualization experiments. The theory allows for a description of the interaction between the main body of the flow, driven by inertial and bouyancy forces, and a thin viscous layer near the hump. In the linear frame, it leads to an evaluation of some conditions for having separation in the valley. The experiments have been performed in a small recirculating channel. In the approach flow, there is a well-developed laminar boundary layer with a height of the same order of that of the obstacle, and constant stable stratification. The Froude number (based on obstacle height) has been varied from 0.25 to 1.8. The two ridges are of small to moderate slope (between 1\4 and 1\2); the distance D between them varies between being slightly less than to much greater than the wavelength of internal gravity waves or lee waves. The experimental results confirm the general prediction of linear theory that for typical valley slopes, some separated or recirculating flow generally occurs in the valley between the ridges. Both theory and the experiments suggest that over a narrow range of Froude number F L (based on the hump half length L) such that the natural lee wavelength is about equal to the valley width D, and for a particular ratio D/L of about 6, the valley is ‘ventilated’, i.e., there is no significant region of separation. This result is different if strong resonant modes are excited, associated with an elevated inversion. In general, the surface winds are expected to be greatest on the lee slope of the second hump. These results extend and confirm previous estimates for valley flows in stably stratified airstreams.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 40 (1987), S. 295-307 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Conditions for separation of a cross flow over a two-dimensional periodic valley are derived from linearized laminar and turbulent boundary-layer models. The results are compared with the predictions of numerical computations and from published laboratory data. Some results for isolated valleys are also discussed.
    Type of Medium: Electronic Resource
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  • 10
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    Unknown
    CNR-DTA
    In:  EPIC311th Ny-Alesund Science Managers Committee Seminar; National Research Council of Italy, Rome, Italy, 9 - 11 October 2013 ; abstracts, (Publications. Department of Earth System Science and Environmental Technologies (DTA). CNR), Rome, Italy, CNR-DTA, 122 p., ISBN: ISSN 2239-5172
    Publication Date: 2014-12-10
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev , info:eu-repo/semantics/other
    Format: application/pdf
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