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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Micrometeorology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (254 pages)
    Edition: 1st ed.
    ISBN: 9783642545450
    DDC: 551.66
    Language: English
    Note: Intro -- Preface -- Contents -- Abbreviations -- Symbols -- 1 History and Definition -- 1.1…Micrometeorological Measurements -- 1.2…Towards the Footprint Definition -- 1.3…Footprint Modeling -- 1.4…Validation of Footprint Models -- References -- 2 Surface-Layer Properties and Parameterizations -- 2.1…Atmospheric Boundary Layer and Scales -- 2.2…Turbulence Parameterization -- 2.2.1 Flux-Gradient Similarity -- 2.2.2 Profile Functions Above the Canopy -- 2.2.3 Profile Functions in the Canopy -- 2.2.4 Roughness Sublayer -- 2.2.5 Power Laws -- 2.2.6 Dispersion Profiles -- 2.2.7 Relevance of Profile Parameterizations in Footprint Models -- 2.3…Internal Boundary Layers -- 2.3.1 Mechanical Internal Boundary Layer -- 2.3.2 Thermal Internal Boundary Layer -- 2.3.3 Blending Height Concept -- 2.4…Modeling Concepts -- 2.4.1 Diffusion Model -- 2.4.2 Lagrangian Model -- 2.4.3 Higher-Order Closure Model -- 2.4.4 Large-Eddy Simulation Model -- 2.5…Averaging Surface Characteristics -- 2.5.1 Averaging Using Effective Parameters -- 2.5.2 Flux-Averaging Models in Inhomogeneous Terrain -- References -- 3 Classification of Footprint Models -- 3.1…Analytical Footprint Models -- 3.1.1 The Schuepp et al. (1990) Approach -- 3.1.2 The Schmid and Oke (1990) approach -- 3.1.3 The Family of Horst and Weil's (1992) Analytical Solution -- 3.1.3.1 The Horst and Weil (1992, 1994) Approach -- 3.1.3.2 The Schmid (1994, 1997) Approaches -- 3.1.3.3 The Kaharabata et al. (1997) Approach -- 3.1.3.4 The Haenel and Grünhage (1999) approach -- 3.1.3.5 The Kormann and Meixner (2001) Approach -- 3.1.4 Analytical Solutions Based on Lagrangian Models -- 3.2…Lagrangian Simulations -- 3.2.1 The Leclerc and Thurtell (1990) Approach -- 3.2.2 The Sabelfeld-Rannik Approach -- 3.2.3 The Kljun et al. (2002) 3D Backward Lagrangian Footprint Model -- 3.3…Higher-Order Closure Footprint Models. , 3.4…Large-Eddy Simulation Models -- 3.5…Hybrid Footprint Models -- 3.5.1 LES-Driven Lagrangian Stochastic Models -- 3.5.1.1 The Prabha et al. (2008) Approach -- 3.5.1.2 The Cai and Leclerc (2007) and Cai et al. (2008) Approach -- 3.5.2 LES-Embedded Lagrangian Stochastic Models: The Steinfeld et al. (2008) Approach -- 3.5.3 Higher-Order Closure-Driven Lagrangian Simulation -- 3.5.3.1 The Luhar and Rao (1994) Approach -- 3.5.3.2 The Hsieh and Katul (2009) Approach -- 3.5.3.3 E- omega Model Closure-Driven Lagrangrian Simulation -- References -- 4 Footprint Studies -- 4.1…Footprint in the Atmospheric Boundary Layer -- 4.1.1 Tall Tower Footprints -- 4.1.2 The Influence of Coriolis Forces on Footprint -- 4.1.3 Flux Footprints in the Convective Boundary Layer -- 4.1.4 Footprint in the Roughness Sub-Layer of Plant Canopies -- 4.2…In-Canopy Footprints -- 4.3…Flux Footprint in Canopy Over Hills -- 4.4…Influence of Contrasting Adjoining Surfaces on Footprints -- 4.4.1 Role of Contrasting Thermal Land Surfaces on Fluxes and Footprints -- 4.4.2 Role of Clearcuts on Forest Fluxes/Footprints -- 4.4.3 Footprints in the Presence of a Transition from the Forest Leading Edge -- 4.5…Flux Footprints Over Complex Topography in Forests -- 4.6…Emissions of Odor and Reactive Trace Gas Fluxes Using the Flux Footprint Method -- 4.7…Footprints in Urban Areas -- References -- 5 Model Validation -- 5.1…Model Validation Against Other Models -- 5.2…Model Validation and Comparison Against Experimental Data -- 5.3…Model Validation with Natural Tracers -- 5.4…Classification of the Comparison Results -- References -- 6 Land Surface: Coupled Footprints -- 6.1…Grid Schema of Surface Characteristics -- 6.2…Determination of Surface Characteristics -- 6.2.1 Roughness Length -- 6.2.2 Remote-Sensing Data -- 6.3…Coupling Footprint Results with Surface Information -- References. , 7 Application of Footprint Models to Different Measurement Techniques -- 7.1…Profile Technique -- 7.1.1 Profile Technique with Three and More Measuring Levels -- 7.1.2 Profile Technique with Two Measuring Levels -- 7.1.3 Accuracy and Footprint Issues for Profile Technique -- 7.1.3.1 Accuracy of Profile Measurements -- 7.1.3.2 Footprint of Profile Measurements -- 7.2…Eddy--Covariance Technique -- 7.2.1 Basics of the Eddy-Covariance Method -- 7.2.2 1D Eddy-Covariance Method -- 7.2.3 Generalized Eddy-Covariance Method (3D) -- 7.2.4 Quality Control of Eddy-Covariance Data -- 7.3…Scintillometer Technique -- 7.4…Airborne Measurement Technique -- References -- 8 Practical Applications of Footprint Techniques -- 8.1…Selection of Flux Measurement Sites -- 8.2…Interpretation of Flux Data -- 8.2.1 Footprint Climatology -- 8.2.2 Covering the Area of Interest -- 8.2.3 Footprint-Dependent Data Quality Control -- 8.3…Upscaling Point Measurements Using Footprint Models -- 8.4…Additional Practical Application -- 8.4.1 Air Pollution Application and Trace Gas Fluxes -- 8.4.2 Wind-Energy Application -- 8.5…Easily Applicable Footprint Models -- 8.6…Limits of Footprint Application -- References -- 9 Looking Forward to the Next Generation of Footprint Models -- References -- Glossary -- About the Authors -- Index.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 71 (1994), S. 169-187 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Temperature fluctuations in a convective surface layer were investigated. Box counting analysis was performed to investigate fractal properties of surfaces of constant temperature and was performed on sets of points obtained by setting thresholds on detrended records. Results indicate that surfaces of constant temperature have fractal properties for thresholds far from the mean. Estimated fractal dimensions of one-dimensional cuts through these surfaces varied between 0.23 and 0.66, increasing with threshold value approaching the mean temperature. For thresholds close to the mean, no fractal behavior was found. Asymmetry in results for thresholds above and below the mean temperature was attributed to the asymmetry between updrafts and downdrafts in the convective surface layer. The temperature dissipation rate (TD) was also investigated. It was found to be strongly intermittent with large fluctuations of the intermittency exponent. Moments were analyzed in order to investigate multifractal properties of TD. Results indicate scaling in the range of 50η–1000η (where η is the Kolmogorov scale) and multifractal properties resembling those observed for passive scalar dissipation in laboratory flows.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract This paper reports on forced-convection mass transfer from isolated discs on rectangular plates as well as hemispheres on realistic fluttering leaves. An electrochemical method was used where the convective transfer of ions to the test electrode (the droplet or the wet spot) in an electrolytic flow system was measured as a function of flow rates, sizes of discs and hemispheres. Measurements showed that the local transfer coefficient for uniformly transferring plates varied as expected while the transfer from isolated discs on plates was much less a function of the distance from the leading edge. An expression to describe the transfer coefficient for an isolated disc as a function of distance from the leading edge was determined. An expression describing the transfer from hemispherical drops on fluttering leaves was derived and compared with the predictions from transfer theory for a sphere in free space.
    Type of Medium: Electronic Resource
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