Analyses of turbulence in the neutrally and stably stratified planetary boundary layer

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Bibliographic Details
Main Author: Ansorge, Cedrick, (Author)
Format: eBook
Language: English
Published: Cham, Switzerland : Springer, [2016]
Series: Springer theses,
Subjects:
ISBN: 9783319450445
9783319450438
Physical Description: 1 online resource (xxi, 171 pages) : illustrations (some color)

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Table of contents

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020 |a 9783319450445  |q (electronic bk.) 
020 |z 9783319450438  |q (print) 
024 7 |a 10.1007/978-3-319-45044-5  |2 doi 
035 |a (OCoLC)958933175  |z (OCoLC)958865091  |z (OCoLC)959424925 
100 1 |a Ansorge, Cedrick,  |e author. 
245 1 0 |a Analyses of turbulence in the neutrally and stably stratified planetary boundary layer /  |c Cedrick Ansorge. 
264 1 |a Cham, Switzerland :  |b Springer,  |c [2016] 
264 4 |c ©2017 
300 |a 1 online resource (xxi, 171 pages) :  |b illustrations (some color) 
336 |a text  |b txt  |2 rdacontent 
337 |a počítač  |b c  |2 rdamedia 
338 |a online zdroj  |b cr  |2 rdacarrier 
490 1 |a Springer theses,  |x 2190-5053 
500 |a "Doctoral thesis accepted by University of Hamburg, Hamburg, Germany." 
504 |a Includes bibliographical references and index. 
505 0 |a Supervisor's Foreword; Parts of this thesis have been published in the following journal articles: ; Acknowledgments; Contents; Symbols and Abbreviations; Persons Mentioned in This Work; Part I Preliminaries; 1 Introduction; 1.1 Turbulence Regimes; 1.2 Global Intermittency; 1.3 Approaches to Studying the Stable Boundary Layer; 1.4 Research Proposition; References; 2 Problem Formulation and Tools; 2.1 The Governing Equations; 2.2 Non-dimensionalization and Parameter Space; 2.2.1 The Neutrally Stratified Regime; 2.2.2 Uniqueness of the Solution. 
505 8 |a 2.2.3 Imposing Stratification: Initial and Boundary Conditions2.2.4 Parameter Space of the Non-dimensionalized Problem; 2.3 Analysis Tools; 2.3.1 Conditional Sampling; 2.3.2 Temporally Resolved Probes; 2.4 Summary; References; Part II Numerics; 3 Discretization; 3.1 The Pressure Problem; 3.2 Spatial Discretization; 3.3 Time Stepping Schemes; 3.3.1 Explicit Runge -- Kutta Schemes; 3.3.2 Semi-implicit Runge -- Kutta Schemes; 3.3.3 Multi-level Schemes and Other Methods; 3.3.4 Choice of a Method; 3.4 Stability of the SIRK3 Scheme; 3.5 Implementation of the SIRK3 Scheme. 
505 8 |a 3.5.1 Rotation of the Grid: Equations Solved by the DNS3.5.2 Buffer Zone; 3.5.3 Discretization in the Interior of the Domain; 3.5.4 Dirichlet Boundary Conditions for the Semi-implicit Solver; 3.5.5 Integration of a Scalar Variable; 3.5.6 Description of the Implementation; References; 4 Overlapping Communication and Computation; 4.1 Motivation -- A Rough Estimate of the Computational Demand; 4.1.1 Memory Demand; 4.1.2 Computational Demand; 4.1.3 The Link Between Spatial Discretization and Communication; 4.2 Approach and Implementation; 4.2.1 Why Overlap Communication and Computation? 
505 8 |a 4.2.2 Design of the NB3DFFT Library4.2.3 Re-Organization of the Algorithm; 4.3 Performance Measurements; 4.3.1 Performance Metrics: Strong and Weak Scaling; 4.3.2 Performance on the Supercomputer juqueen; References; 5 A Test Bed for the Numerical Tool; 5.1 Behavior of the Semi-implicit Scheme When Solving a Non-linear ODE; 5.2 Analytical Solution of Ekman Flow; 5.2.1 The Stationary Laminar Solution; 5.2.2 Temporally Evolving Solution; 5.2.3 Convergence of the Errors; 5.3 Two-Dimensional Taylor -- Green Vortex; 5.4 Three-Dimensional Turbulent Ekman Layer; References; Part III Physics. 
505 8 |a 6 The Neutrally Stratified Ekman Layer6.1 Conventional Statistics; 6.1.1 Global Measures; 6.1.2 Vertical Profiles; 6.2 Local Versus Ensemble Statistics; 6.2.1 Data Analysis Procedure; 6.2.2 Convergence of local estimates to the ensemble mean; 6.3 External Intermittency and Its Impact in the Surface Layer; 6.3.1 Definition of external intermittency; 6.3.2 A Vorticity Source in the Outer Layer; 6.3.3 A Modified Logarithmic Law for the Mean Velocity; 6.4 Flow Synopsis; 6.5 Summary; References; 7 Turbulence Regimes and Stability; 7.1 Initial Conditions and Time Scales Under Stable Stratification. 
506 |a Plný text je dostupný pouze z IP adres počítačů Univerzity Tomáše Bati ve Zlíně nebo vzdáleným přístupem pro zaměstnance a studenty 
590 |a SpringerLink  |b Springer Complete eBooks 
650 0 |a Boundary layer (Meteorology)  |x Mathematical models. 
650 0 |a Turbulent boundary layer. 
655 7 |a elektronické knihy  |7 fd186907  |2 czenas 
655 9 |a electronic books  |2 eczenas 
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830 0 |a Springer theses,  |x 2190-5053 
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