ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer Academic Publ.
    Call number: MOP 47358 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XII, 666 S. : Ill., graph. Darst.
    ISBN: 9027727686
    Series Statement: Atmospheric Sciences Library
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer
    Call number: PIK N 456-93-0121
    Type of Medium: Monograph available for loan
    Pages: XII, 666 S. : Ill., graph. Darst.
    Edition: 2. repr.
    ISBN: 9027727686 , 90-277-2769-4
    Series Statement: Atmospheric and oceanographic sciences library 13
    Location: A 18 - must be ordered
    Branch Library: PIK Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Monograph available for loan
    Monograph available for loan
    Minneapolis [u.a.] : West Publ. Comp.
    Call number: AWI A5-97-0239
    Type of Medium: Monograph available for loan
    Pages: XIII, 385 S. : zahlr. graph. Darst.
    ISBN: 0314064710
    Note: Contents: 1The Atmosphere. - Meteorological Conventions. - [Focus: Descartes and the Scientific Method]. - Thermodynamic State. - Pressure. - Density. - Temperature. - [Focus: Escape Velocity]. - Equation of State - Ideal Gas Law. - Hydrostatic Equilibrium. - Hypsometric Equation. - Atmospheric Structure. - Standard Atmosphere. - Layers of the Atmosphere. - Process Terminology. - Summary. - Exercises. - 2 Heat. - Flux. - Radiation Principles. - Propagation. - Emission. - Distribution. - Absorption, Reflection & Transmission. - Sensible and Latent Heats. - Sensible. - Latent. - Lagrangian Heat Budget. - First Law of Thermodynamics. - Lapse Rate. - Adiabatic Lapse Rate. - Potential Temperature. - Thermodynamic Diagrams - Part 1: Dry Adiabatic Processes. - [Focus: Spreadsheet Thermodynamics]. - Mean and Turbulent Parts. - Eulerian Heat Budget. - First Law of Thermodynamics - Revisited. - Advection. - Turbulence. - Conduction & Surface Fluxes. - Radiation. - Net Heat Budget. - Summary. - Exercises. - Temperature. - Astronomical Factors. - Planetary Orbits. - Orbit of the Earth. - Seasonal Effects. - Daily Effects. - Sunrise, Sunset & Twilight. - Average Daily Insolation. - Surface Radiation Budget. - Solar. - Longwave (IR). - Net Radiation. - Surface Heat and Moisture Budgets. - Heat Budget. - Bowen Ratio. - Moisture Budget. - Cumulative Heating or Cooling. - Nighttime. - Daytime. - Static Stability - a preview. - Boundary Layer. - Definitions. - Structure. - Temperature-Profile Evolution. - Stable-Boundary-Layer Temperature. - Mixed-Layer Temperature. - Wind Chill. - Summary. - Exercises. - 4 Optics. - Ray Geometry. - Reflection. - Refraction. - Huygen's Principle. - Critical Angle. - [Focus: Newton and Calors]. - Liquid Drop Optics. - Reflection from Water. - Primary Rainbow. - Secondary Rainbow. - Alexander's Dark Band. - [Focus: Rainbows and the Renaissance]. - Ice-Crystal Optics. - Sun Pillar. - Parhelle Circle. - Subsun. - 22° Halo. - 46° Halo. - Circumzenith Arc. - Sun Dogs. - Subsun Dogs. - Upper Tangent Ares. - Scattering. - Rayleigh Scattering. - Polarization. - Geometric Scattering. - Mie Scattering. - [Focus: Great Scientists Make Big Mistakes]. - Diffraction. - Mirages. - Summary . - Exercises. - 5 Moisture. - Saturation Vapor Pressure. - Vapor Pressure. - Saturation. - Humidity Variables. - Mixing Ratio. - Specific Hurnidity. - Absolute Humidity. - Relative Hurnidity. - Dew Point Temperature. - Saturation Level or Lifting Condensation Level (LCL). - Wet-Bulb Temperature. - More Relationships Between Moisture Variables. - Saturated Adiabatic Lapse Rate. - Thermo Diagrams - Part 2: Moisture. - Isohurnes. - Moist (Saturated) Adiabats. - Summary. - Exercises. - 6 Clouds. - Cloud Condensation Nuclei (CCN). - Terminal Velocity of Cloud Droplets. - Cloud Sizes. - Fractal Cloud Shapes. - Fractal Dimension. - Measuring Fractal Dimension. - Water Budget. - Total Water. - Eulerian Budget. - Lagrangian Budget. - Processes Causing Saturation. - Cooling and Moisturizing. - Mixing. - Clouds and Upslope Fog. - Other Fogs. - Processes. - Formation and Growth. - Evolution of Radiation Fog. - Dissipation of Weil-Mixed Fogs. - Satellite Orbits. - Summary. - Exercises. - 7 Stability. - Thermodynamic Diagrams-Part 3: Applications. - State. - Dry (Unsaturated) Processes. - Moist (Saturated) Processes & Liquid Water. - Precipitation. - Parcels vs. Environment. - Buoyancy. - Thermo Diagrams for Boundary Layers. - Static Stability. - Unstable. - Neutral. - Stahle. - Mixed-Layer Depth. - Brünt-Väisälä Frequency. - Dynamic Stability. - Cloud Development. - Active. - Passive. - Summary. - Exercises. - 8 Precipitation. - [Focus: Meteorsand Meteorology]. - Nucleation of Liquid Droplets. - Curvature and Solute Effects. - Critical Radius. - Haze. - Activated Nuclei. - Nucleation of Ice Crystals. - Processes. - Nuclei. - Droplet Growth by Diffusion. - Max Droplet Radius via Diffusion. - Growth Rate. - Ice Growth by Diffusion. - Ice Crystal Habits. - Growth Rates. - The Wegener-Bergeron-Findeisen (WBF) Process. - Collision & Collection. - Processes. - Droplet Size Distributions. - Terminal Velocity of Precipitation. - Precipitable Water. - Rainfall Rate Estimated by Radar. - Summary. - Exercises. - 9 Dynamics. - Newton's Second Law of Motion. - Equations of Motion. - Advection. - Pressure Gradient Force. - Coriolis Force. - Turbulent Drag Force. - Centrifugal Force. - Full Equations. - Balance of Forces. - Geostrophic Wind. - Gradient Wind. - Boundary-Layer Wind. - Full Equations of Motion- Revisited Mass Conservation. - Continuity Equation. - Boundary-Layer Pumping. - Summary. - Exercises. - 10 Local Winds. - Scales of Motion. - Wind-Speed Probability. - Wind Turbines and Power GenerationThermals. - Katabatic Wind. - Surface-Layer Winds. - Roughness Length. - Log Wind Profile. - Skin Drag. - Turbulence Intensity. - Scaling Velocities. - Velocity Standard Deviation. - Turbulence Kinetic Energy. - Mountain Waves. - Natural Wavelength. - Lenticular Clouds. - Froude Number. - Mountain-Wave Drag. - Foehns and Chinooks. - Summary. - Exercises. - 11Global Circulation. - Nomenclature. - Differential Heating. - Meridional Temperature Gradient. - Radiative Forcings. - Heat Transport Needed. - Thermal Wind Relationship. - Jet Stream. - Baroclinicity. - Angular Momentum. - Vorticity. - Relative Vorticity. - Absolute Vorticity. - Potential Vorticity. - Isentropic Potential Vorticity. - Midlatitude Cyclones and Anticyclones. - Barotropic Instability & Rossby Waves. - Baroclinic Instability & Planetary Waves. - Heat Transport. - Momentum Transport . - Three-Band General Circulation. - Ekman Spiral in the Ocean. - Summary. - Exercises. - 12 Air Masses & Fronts. - Anticyclones or Highs. - Air Masses. - Creation. - Modification. - Synoptic Weather Maps. - Weather Observations. - Map Analysis, Plotting & Isoplething. - Surface Fronts. - Horizontal Structure. - Geostrophic Adjustment. - Vertical Structure. - Frontogenesis. - Kinematics. - Thermodynamics. - Dynamics. - Upper-Level Fronts. - Dry Lines. - Summary. - Exercises. - 13 Cyclones. - Case Study of a Cyclone over North America. - Overview and Storm Track. - Storm Data. - Cyclogenesis. - Lee Cyclogenesis. - Stationary Planetary Waves. - Conservation of Potential Vorticity. - Equatorward Propagation Along the Lee Side. - Cyclone Spin-Up. - Vorticity Tendency. - Quasigeostrophic Approximation. - Application to Typical Weather Patterns. - Upward Motion. - Jet-Stream Curvature. -Jet Streaks. - Sea-level Pressure Tendency. - Mass Budget. - Diabatic Heating. - Evolution. - Iso-surfaces and Their Utility. - Height. - Pressure. - Thickness. - Potential Temperature. - Potential Vorticity (PVU). - Self Development of Cyclones. - Condensation. - Temperature Advection. - Case Study of a Cyclone (continued). - Summary. - Exercises. - 14 Numerical Weather Prediction. - Solutions to Atmospheric Equations. - [Focus: History of NWP]. - Grid Points. - Finite-Difference Equations. - Numerical Stability. - The Numerical-Forecast Process. - Balanced Mass and Flow Fields. - Data Assimilation and Analysis. - Forecasts. - [Focus: Electricity & Operational Reliability]. - Case Study: 22-25 Feb 1994 - N. America. - Post-processing. - Forecast Refinement. - Forecast Quality. - Accuracy vs. Skill. - Verification Scores. - Nonlinear Dynamics and Chaos. - Predictability. - Lorenz Strange Attractor. - [Focus: Lorenz and Scientific Revolutions]. - Ensemble Forecasts. - Useful Indicators on Weather Maps. - Elements of a Good Weather Briefing. - Summary. - Exercises. - 15 Thunderstorms. - Convective Conditions. - Conditional Instability. - Trigger Mechanisms. - CAPE. - Severe-Thunderstorm Environment . - Downbursts and Gust Fronts. - Precipitation Drag. - Evaporative Cooling. - [Focus: Downbursts & Flight Operations]. - Gust Fronts. - Lightning and Thunder. - Lightning. - Thunder. - Tornadoes. - Origin of Rotation. - Mesocyclones and Helicity. - Tornadoes and Swirl Ratio
    Location: AWI Reading room
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer
    Call number: PIK N 456-93-0048
    Type of Medium: Monograph available for loan
    Pages: XII, 666 S. : Abb. ; 24 cm
    ISBN: 9027727694
    Series Statement: Atmospheric Sciences Library
    Location: A 18 - must be ordered
    Branch Library: PIK Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Monograph available for loan
    Monograph available for loan
    Dordrecht : Kluwer
    Associated volumes
    Call number: AWI A7-92-0297
    In: Atmospheric sciences library, 13
    Description / Table of Contents: Part of the excitement in boundary-layer meteorology is the challenge associated with turbulent flow - one of the unsolved problems in classical physics. The flavor of the challenges and the excitement associated with the study of the atmospheric boundary layer are captured in this textbook. The work should also be considered as a major reference and as a review of the literature, since it includes tables of parameterizations, procedures, field experiments, useful constants, and graphs of various phenomena under a variety of conditions. The author envisions, and has catered for, a heterogeneity in the background and experience of his readers. Therefore, the book is useful to beginning graduate students as well as established scientists.
    Type of Medium: Monograph available for loan
    Pages: XII, 666 Seiten , Illustrationen
    ISBN: 9027727686 , 90-277-2769-4
    Series Statement: Atmospheric sciences library 13
    Language: English
    Note: Contents Preface 1 Mean Boundary Layer Characteristics 1.1 A boundary-layer definition 1.2 Wind and flow 1.3 Turbulent transport 1.4 Taylor's hypothesis 1.5 Virtual potential temperature 1.6 Boundary layer depth and structure 1.7 Micrometeorology 1.8 Significance of the boundary layer 1.9 General references 1.10 References for this chapter 1.11 Exercises 2 Some Mathematical and Conceptual Tools: Part 1. Statistics 2.1 The significance of turbulence and its spectrum 2.2 The spectral gap 2.3 Mean and turbulent parts 2.4 Some basic statistical methods 2.5 Turbulence kinetic energy 2.6 Kinematic flux 2.7 Eddy flux 2.8 Summation notation 2.9 Stress 2.10 Friction velocity 2.11 References 2.12 Exercises 3 Application of the Governing Equations to Turbulent Flow 3.1 Methodology 3.2 Basic governing equations 3.3 Simplifications, approximations, and scaling arguments 3.4 Equations for mean variables in a turbulent flow 3.5 Summary of equations, with simplifications 3.6 Case studies 3.7 References 3.8 Exercises 4 Prognostic Equations for Turbulent Fluxes and Variances 4.1 Prognostic equations for the turbulent departures 4.2 Free convection scaling variables 4.3 Prognostic equations for variances 4.4 Prognostic equations for turbulent fluxes 4.5 References 4.6 Exercises 5 Turbulence Kinetic Energy, Stability, and Scaling 5.1 The TKE budget derivation 5.2 Contributions to the TKE budget 5.3 TKE budget contributions as a function of eddy size 5.4 Mean kinetic energy and its interaction with turbulence 5.5 Stability concepts 5.6 The Richardson number 5.7 The Obukhov length 5.8 Dimensionless gradients 5.9 Miscellaneous scaling parameters 5.10 Combined stability tables 5.11 References 5.12 Exercises 6 Turbulence Closure Techniques 6.1 The closure problem 6.2 Parameterization rules 6.3 Local closure - zero and half order 6.4 Local closure - first order 6.5 Local closure - one-and-a-half order 6.6 Local closure - second order 6.7 Local closure - third order 6.8 Nonlocal closure - transilient turbulence theory 6.9 Nonlocal closure - spectral diffusivity theory 6.10 References 6.11 Exercises 7 Boundary Conditions and External Forcings 7.1 Effective surface turbulent flux 7.2 Heat budget at the surface 7.3 Radiation budget 7.4 Fluxes at interfaces 7.5 Partitioning of flux into sensible and latent portions 7.6 Flux to and from the ground 7.7 References 7.8 Exercises 8 Some Mathematical and Conceptual Tools: Part 2. Time Series 8.1 Time and space series 8.2 Autocorrelation 8.3 Structure function 8.4 Discrete Fourier transform 8.5 Fast Fourier Transform 8.6 Energy spectrum 8.7 Spectral characteristics 8.8 Spectra of two variables 8.9 Periodogram 8.10 Nonlocal spectra 8.11 Spectral decomposition of the TKE equation 8.12 References 8.13 Exercises 9 Similarity Theory 9.1 An overview 9.2 Buckingham Pi dimensional analysis methods 9.3 Scaling variables 9.4 Stable boundary layer similarity relationship lists 9.5 Neutral boundary layer similarity relationship lists 9.6 Convective boundary layer similarity relationship lists 9.7 The log wind profile 9.8 Rossby-number similarity and profile matching 9.9 Spectral similarity 9.10 Similarity scaling domains 9.11 References 9.12 Exercises 10 Measurement and Simulation Techniques 10.1 Sensor and measurement categories 10.2 Sensor lists 10.3 Active remote sensor observations of morphology 10.4 Instrument platforms 10.5 Field experiments 10.6 Simulation methods 10.7 Analysis methods 10.8 References 10.9 Exercises 11 Convective Mixed Layer 11.1 The unstable surface layer 11.2 The mixed layer 11.3 Entrainment zone 11.4 Entrainment velocity and its parameterization 11.5 Subsidence and advection 11.6 References 11.7 Exercises 12 Stable Boundary Layer 12.1 Mean Characteristics 12.2 Processes 12.3 Evolution 12.4 Other Depth Models 12.5 Low-level (nocturnal) jet 12.6 Buoyancy (gravity) waves 12.7 Terrain slope and drainage winds 12.8 References 12.9 Exercises 13 Boundary Layer Clouds 13.1 Thermodynamics 13.2 Radiation 13.3 Cloud entrainment mechanisms 13.4 Fair-weather cumulus 13.5 Stratocumulus 13.6 Fog 13.7 References 13.8 Exercises 14 Geographic Effects 14.1 Geographically generated local winds 14.2 Geographically modified flow 14.3 Urban heat island 14.4 References 14.5 Exercises Appendices A. Scaling variables and dimensionless groups B. Notation C. Useful constants, parameters and conversion factors D. Derivation of virtual potential temperature Subject Index
    Location: AWI Reading room
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 62 (1993), S. 21-96 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Some of the larger eddies in a turbulent region can be coherent structures that turbulently advect air parcels across large vertical distances before smaller eddies mix the parcels with the environment. Such a process is nonlocal rather than diffusive. Transilient turbulence theory, named after a Latin word maaning “jump over”, provides a framework for considering the ensemble-averaged effect of many eddies of different sizes on the net nonlocal mixing in the vertical. Nonlocal turbulence statistics can then be examinated, and nonlocal first-order closure can be formulated.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 55 (1991), S. 67-90 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The parameterization for transilient turbulence coefficients suggested by Stull and Driedonks (SD. 1987) is tested against the large-eddy simulations (LES) of Ebert et al. (ESS, 1989) for the special case of an idealized convective boundary layer. The SD parameterization is based on a nonlocal approximation to the turbulence kinetic energy (TKE) equation, and requires turbulent exchange (i.e., the matrix of transilient mixing coefficients is assumed to be symmetric) and dominance of the smaller eddies (i.e., elements closer to the main diagonal of the matrix are greater). Measurements from the LES model, however, show that the transilient matrix is asymmetric in convective situations, with larger eddies dominating. Mean-state conditions such as the deep convective mixing and mixed-layer growth are satisfactorily described by the parameterization, but the surface layer is too deep and the entrainment zone thickness is poorly defined. Turbulence properties such as skewed vertical velocity distributions are not possible within the constraint of a symmetric matrix, and partial convective overturning is also not possible because of the restriction that small eddies dominate. Future improved parametcrizations might continue to be based on the TKE equation, but should allow transilient matrix asymmetry.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 1993-01-01
    Print ISSN: 0006-8314
    Electronic ISSN: 1573-1472
    Topics: Geosciences , Physics
    Published by Springer
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 1991-04-01
    Print ISSN: 0006-8314
    Electronic ISSN: 1573-1472
    Topics: Geosciences , Physics
    Published by Springer
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2006-11-01
    Print ISSN: 0168-1923
    Electronic ISSN: 1873-2240
    Topics: Geography , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition , Physics
    Published by Elsevier
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...