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  • 1
    Monograph available for loan
    Monograph available for loan
    Chichester : Wiley Blackwell
    Call number: AWI A6-15-0020
    Description / Table of Contents: This book gives a coherent development of the current understanding of the fluid dynamics of the middle latitude atmosphere. lt is primarily aimed at post-graduate and advanced undergraduate level students and does not assume any previous knowledge of fluid mechanics, meteorology or atmospheric science. The book will be an invaluable resource for any quantitative atmospheric scientist who wishes to increase their understanding of the subject. The importance of the rotation of the Earth and the stable stratification of its atmosphere, with their implications for the balance of larger-scale flows, is highlighted throughout. Clearly structured throughout, the first of three themes deals with the development of the basic equations for an atmosphere on a rotating, spherical planet and discusses scale analyses of these equations. The second theme explores the importance of rotation and introduces vorticity and potential vorticity, as well as turbulence. In the third theme, the concepts developed in the first two themes are used to give an understanding of balanced motion in real atmospheric phenomena. lt starts with quasi-geostrophic theory and moves on to linear and nonlinear theories for mid-latitude weather systems and their fronts. The potential vorticity perspective on weather systems is highlighted with a discussion of the Rossby wave propagation and potential vorticity mixing covered in the final chapter.
    Type of Medium: Monograph available for loan
    Pages: XVIII, 408 Seiten , Illustrationen
    ISBN: 9780470795194
    Series Statement: Advancing weather and climate science
    Language: English
    Note: Contents: Series foreword. - Preface. - Select bibliography. - The authors. - 1 Observed flow in the Earth's midlalitudes. - 1.1 Vertical structure. - 1.2 Horizontal structure. - 1.3 Transient activity. - 1.4 Scales of motion. - 1.5 The Norwegian frontal model of cyclones. - Theme 1 Fluid dynamics of the midlatitude atmosphere. - 2 Fluid dynamics in an inertial frame of reference. - 2.1 Definition of fluid. - 2.2 Flow variables and the continuum hypothesis. - 2.3 Kinematics: characterizing fluid flow. - 2.4 Governing physical principles. - 2.5 Lagrangian and Eulerian perspectives. - 2.6 Mass conservation equation. - 2.7 First Law of Thermodynamics. - 2.8 Newton's Second Law of Motion. - 2.9 Bernoulli's Theorem. - 2.10 Heating and water vapour. - 3 Rotating frames of reference. - 3.1 Vectors in a rotating frame of reference. - 3.2 Velocity and Acceleration. - 3.3 The momentum equation in a rotating frame. - 3.4 The centrifugal pseudo-force. - 3.5 The Coriolis pseudo-force. - 3.6 The Taylor-Proudman theorem. - 4 The spherical Earth. - 4.1 Spherical polar coordinates. - 4.2 Scalar equations. - 4.3 The momentum equations. - 4.4 Energy and angular momentum.- 4.5 The shallow atmosphere approximation. - 4.6 The beta effect and the spherical Earth. - 5 Scale analysis and its applications. - 5.1 Principles of scaling methods. - 5.2 The use of a reference atmosphere. - 5.3 The horizontal momentum equations. - 5.4 Natural coordinates, geostrophic and gradient wind balance. - 5.5 Vertical motion. - 5.6 The vertical momentum equation. - 5.7 The mass continuity equation. - 5.8 The thermodynamic energy equation. - 5.9 Scalings for Rossby numbers that are not small. - 6 Alternative vertical coordinates. - 6.1 A general vertical coordinate. - 6.2 Isobaric coordinates. - 6.3 Other pressure-based vertical coordinates. - 6.4 Isentropic coordinates. - 7 Variations of density and the basic equations. - 7.1 Boussinesq approximation. - 7.2 Anelastic approximation. - 7.3 Stratification and gravity waves. - 7.4 Balance, gravity waves and Richardson number. - 7.5 Summary of the basic equation sets. - 7.6 The energy of atmospheric motions. - Theme 2 Rotation in the atmosphere. - 8 Rotation in the atmosphere. - 8.1 The concept of vorticity. - 8.2 The vorticity equation. - 8.3 The vorticity equation for approximate sets of equations. - 8.4 The solenoidal term. - 8.5 The expansion/contraction term. - 8.6 The stretching and tilting terms. - 8.7 Friction and vorticity. - 8.8 The vorticity equation in alternative vertical coordinates. - 8.9 Circulation. - 9 Vorticity and the barotropic vorticity equation. - 9.1 The barotropic vorticity equation. - 9.2 Poisson's equation and vortex interactions. - 9.3 Flow over a shallow hill. - 9.4 Ekman pumping. - 9.5 Rossby waves and the beta plane. - 9.6 Rossby group velocity. - 9.7 Rossby ray tracing. - 9.8 Inflexion point instability. - 10 Potential vorticity. - 10.1 Potential vorticity. - 10.2 Alternative derivations of Ertel's theorem. - 10.3 The principle of invertibility. - 10.4 Shallow water equation potential vorticity. - 11 Turbulence and atmospheric flow. - 11.1 The Reynolds number . - 11.2 Three-dimensional flow at large Reynolds number. - 11.3 Two-dimensional flow at large Reynolds number. - 11.4 Vertical mixing in a stratified fluid. - 11.5 Reynolds stresses. - Theme 3 Balance in atmospheric flow. - 12 Quasi-geostrophic flows. - 12.1 Wind and temperature in balanced flows. - 12.2 The quasi-geostrophic approximation. - 12.3 Quasi-geostrophic potential vorticity. - 12.4 Ertel and quasi-geostrophic potential vorticities. - 13 The omega equation. - 13.1 Vorticity and thermal advection form. - 13.2 Sutcliffe Form. - 13.3 Q-vector form. - 13.4 Ageostrophic flow and the maintenance of balance. - 13.5 Balance and initialization. - 14 Linear theories of baroclinic instability. - 14.1 Qualitative discussion. - 14.2 Stability analysis of a zonal flow. - 14.3 Rossby wave interpretation of the stability conditions. - 14.4 The Eady model. - 14.5 The Charney and other quasi-geostrophic models. - 14.6 More realistic basic states. - 14.7 Initial value problem. - 15 Frontogenesis. - 15.1 Frontal scales. - 15.2 Ageostrophic circulation. - 15.3 Description of frontal collapse. - 15.4 The semi-geostrophic Eady model. - 15.5 The confluence model. - 15.6 Upper-level frontogenesis. - 16 The nonlinear development of baroclinic waves. - 16.1 The nonlinear domain. - 16.2 Semi-geostrophic baroclinic waves. - 16.3 Nonlinear baroclinic waves on realistic jetson the sphere. - 16.4 Eddy transports and zonal mean flow changes. - 16.5 Energetics of baroclinic waves. - 17 The potential vorticity perspective. - 17.1 Setting the scene. - 17.2 Potential vorticity and vertical velocity. - 17.3 Life cycles of some baroclinic waves. - 17.4 Alternative perspectives. - 17.5 Midlatitude blocking. - 17.6 Frictional and heating effects. - 18 Rossby wave propagation and potential vorticity mixing. - 18.1 Rossby wave propagation. - 18.2 Propagation of Rossby waves into the stratosphere. - 18.3 Propagation through a slowly varying medium. - 18.4 The Eliassen-Palm flux and group velocity. - 18.5 Baroclinic life cycles and Rossby waves. - 18.6 Variations of amplitude. - 18.7 Rossby waves and potential vorticity steps. - 18.8 Potential vorticity steps and the Rhines scale. - Appendices. - Appendix A: Notation. - Appendix B: Revision of vectors and vector calculus. - B.1 Vectors and their algebra. - B.2 Products of vectors. - B.3 Scalar fields and the grad operator. - B.4 The divergence and curl operators. - B.5 Gauss' and Stokes' theorems. - B.6 Some useful vector identities. - Index.
    Location: AWI Reading room
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  • 2
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: AWI A6-94-0200
    Description / Table of Contents: This book gives an account of the modern view of the global circulation of the atmosphere. It brings the observed nature of the circulation together with theories and simple models of the mechanisms which drive it. Early chapters concentrate on the classical view of the global circulation, on the processes which generate atmospheric motions and on the dynamical constraints which modify them. Later chapters develop more recent themes including low frequency variability and the circulations of other planetary atmospheres. The book will be of interest to advanced students and researchers who wish for an introduction to the subject before engaging with the original scientific literature. The book is copiously illustrated, and includes many results of diagnostic and modelling studies. Each chapter includes a set of problems and bibliographical notes.
    Type of Medium: Monograph available for loan
    Pages: XXI, 422 Seiten , Illustrationen
    ISBN: 052141895X
    Series Statement: Cambridge Atmospheric and Space Science Series
    Language: English
    Note: Contents Preface Notation The governing physical laws 1.1 The first law of thermodynamics 1.2 Conservation of matter 1.3 Newton's second law of motion 1.4 Coordinate systems 1.5 Hydrostatic balance and its implications 1.6 Vorticity 1.7 The quasi-geostrophic approximation 1.8 Potential vorticity and the omega equation 1.9 Ertel's potential vorticity 1.10 Problems 2 Observing and modelling global circulations 2.1 Averaging the atmosphere 2.2 The global observing network 2.3 Numerical weather prediction models 2.4 The analysis-forecast cycle 2.5 Global circulation models 2.6 Problems 3 The atmospheric heat engine 3.1 Global energy balance 3.2 Local radiative balance 3.3 Thermodynamics of fluid motion 3.4 Observed atmospheric heating 3.5 Problems 4 The zonal mean meridional circulation 4.1 Observational basis 4.2 The Held-Hou model of the Hadley circulation 4.3 More realistic models of the Hadley circulation 4.4 Zonal mean circulation in midlatitudes 4.5 A Lagrangian view of the meridional circulation 4.6 Problems 5 Transient disturbances in the midlatitudes 5.1 Timescales of atmospheric motion 5.2 The structure of transient eddies 5.3 Atmospheric energetics 5.4 Theories of baroclinic instability 5.5 Baroclinic lifecycles and high frequency transients 5.6 Problems 6 Wave propagation and steady eddies 6.1 Observations of steady eddies 6.2 Barotropic model 6.3 Application to observed steady eddies 6.4 Vertical propagation of Rossby waves 6.5 The Eliassen-Palm flux 6.6 Eliassen-Palm fluxes and baroclinic lifecycles 6.7 Problems 7 Three-dimensional aspects of the global circulation 7.1 Zonal variations in the tropics 7.2 Monsoon circulations 7.3 Midlatitude storm zones and jets 7.4 Interactions between transient and steady eddies 7.5 The global transport of water vapour 7.6 Problems 8 Low frequency variability of the circulation 8.1 Low frequency transients 8.2 Teleconnection-patterns 8.3 Stratospheric oscillations 8.4 Intraseasonal oscillation 8.5 The Southern Oscillation 8.6 Blocking of the midlatitude flow 8.7 Chaos and ultra low frequency variability 8.8 Problems 9 The stratosphere 9.1 The seasonal cycle of the stratospheric circulation 9.2 Wave propagation and mean flow interactions 9.3 The production and transport of ozone 9.4 Exchange of matter across the tropopause 9.5 Problems 10 Planetary atmospheres and other fluid systems 10.1 Major influences on planetary circulations 10.2 Terrestrial circulations 10.3 Slowly rotating atmospheres 10.4 The atmospheric circulation of the giant planets 10.5 Large scale ocean circulation 10.6 Laboratory systems 10.7 Problems Appendix Solutions to Problems Bibliography References Index
    Location: AWI Reading room
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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
    [s.l.] : Nature Publishing Group
    Nature 333 (1988), S. 118-118 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] IN a recent paper1, D. L. Boyer and R.-R. Chen claim that several features of the climate flow in the Northern Hemisphere can be reproduced in a laboratory apparatus. Their experiment involves towing models of the Rockies, Himalayas and Greenland through a rotating tank containing stratified salt ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 338 (1989), S. 619-619 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] SUPERFICIALLY, it can seem that the character of the weather persists in one mode for considerable periods before switching to some very different mode. For example, the early part of this winter was remarkable dry, warm and settled in western Europe. Since mid-February, an equally persistent ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 348 (1990), S. 283-284 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] THE atmosphere undergoes a confusing mixture of random events, with tantalizing glimpses of order which are apt to dissolve even as you look at them. Ramamurthy et al. on page 314 of this issue1 present case studies of one of the more ordered types of event observed in the atmosphere. Using a ...
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  • 7
    Publication Date: 2007-07-01
    Print ISSN: 1545-598X
    Electronic ISSN: 1558-0571
    Topics: Architecture, Civil Engineering, Surveying , Geography , Geosciences
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  • 8
    Publication Date: 1983-07-01
    Print ISSN: 0022-4928
    Electronic ISSN: 1520-0469
    Topics: Geography , Geosciences , Physics
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  • 9
    Publication Date: 2008-08-01
    Print ISSN: 0280-6495
    Electronic ISSN: 1600-0870
    Topics: Geography , Geosciences , Physics
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  • 10
    Publication Date: 2008-08-01
    Print ISSN: 0280-6495
    Electronic ISSN: 1600-0870
    Topics: Geography , Geosciences , Physics
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