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  • 1
    Keywords: Ocean circulation Mathematical models ; Differentiable dynamical systems ; El Niño Current Mathematical models ; Meeresströmung ; El-Niño-Phänomen ; Meereskunde ; Meeresströmung ; Hydromechanik ; Differentiation ; El-Niño-Phänomen ; Southern oscillation ; Meeresströmung ; El-Niño-Phänomen ; Nichtlineares mathematisches Modell
    Type of Medium: Book
    Pages: XVI, 532 S. , Ill., graph. Darst., Kt.
    Edition: 2. rev. and enlarged ed.
    ISBN: 140202262X , 1402022638 , 9781402022630 , 9781402022623
    Series Statement: Atmospheric and oceanographic sciences library 28
    DDC: 551.46/2
    RVK:
    Language: English
    Note: Includes bibliographical references and index
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  • 2
    Keywords: Ocean circulation--Mathematical models. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (469 pages)
    Edition: 1st ed.
    ISBN: 9789401594509
    Series Statement: Atmospheric and Oceanographic Sciences Library ; v.22
    DDC: 551.462
    Language: English
    Note: Front -- Contents -- INTRODUCTION -- BACKGROUND MATERIAL -- A DYNAMICAL SYSTEMS POINT OF VIEW -- NUMERICAL TECHNIQUES -- THE WIND-DRIVEN OCEAN CIRCULATION -- THE THERMOHALINE OCEAN CIRCULATION -- THE DYNAMICS AND PHYSICS OF ENSO -- Index.
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  • 3
    Online Resource
    Online Resource
    New York :Cambridge University Press,
    Keywords: Atmospheric physics. ; Electronic books.
    Description / Table of Contents: This book provides an overview of the applications of complex network theory to climate science. Aimed mainly at researchers and graduate students in climate science, it will also be of value to a broader audience of anyone interested in network science, from biomedicine to ecology to economics.
    Type of Medium: Online Resource
    Pages: 1 online resource (286 pages)
    Edition: 1st ed.
    ISBN: 9781108626682
    DDC: 551.633
    Language: English
    Note: Cover -- Half-title -- Title page -- Copyright information -- Contents -- Preface -- Acknowledgments -- 1 The Climate System -- 1.1 System Components -- 1.2 Forcing -- 1.3 Climate Models -- 1.4 Mean State -- 1.4.1 Atmosphere -- 1.4.2 Ocean -- 2 Climate Variability -- 2.1 Phenomena and Null-Hypothesis -- 2.2 Atmospheric Waves and Teleconnections -- 2.3 The North Atlantic Oscillation -- 2.4 The El Niño-Southern Oscillation -- 2.5 Tropical Circulation and Monsoons -- 2.6 The Atlantic Multidecadal Oscillation -- 3 Climate Data Analysis -- 3.1 Climate Data -- 3.2 Linear Analysis Tools -- 3.2.1 Correlation Analysis -- 3.2.2 Spectral Analysis -- 3.2.3 Wavelets -- 3.2.4 Empirical Orthogonal Functions -- 3.3 Nonlinear Analysis Tools -- 3.3.1 Entropy -- 3.3.2 Mutual Information -- 3.3.3 Event Synchronization -- 3.3.4 Directionality and Causality Measures -- 3.3.5 Ordinal Analysis -- 3.4 Statistical Testing -- 4 Climate Networks: Construction Methods and Analysis -- 4.1 Complex Networks -- 4.1.1 General Definitions and Properties -- 4.1.2 Functional and Structural Networks -- 4.2 Construction of Climate Networks -- 4.2.1 Undirected Network Inferred from SATA -- 4.2.2 Directed Network Inferred from SATA -- 4.3 Climate Communities -- 4.4 Flow Networks -- 4.4.1 Network Description of Lagrangian Transport in Fluid Flows -- 4.4.2 Dispersion, Mixing, and Network Entropies -- 4.4.3 Communities in Flow Networks -- 4.4.4 Optimal Paths in Flow Networks -- 4.4.5 MPP-Betweenness -- 4.5 Event Synchronization Networks -- 5 Computational Tools for Network Analysis -- 5.1 Computational Problem -- 5.2 Serial Tools: pyunicorn -- 5.2.1 Description -- 5.2.2 Performance -- 5.3 Parallel Tools: Par@Graph -- 5.3.1 Description -- 5.3.2 Performance: POP Model Time Series -- 6 Applications to Atmospheric Variability -- 6.1 Network Analysis of ENSO Phases. , 6.2 Evolution of Atmospheric Connectivity in the Twentieth Century -- 6.3 Forced and Internal Atmospheric Variability -- 6.4 Atmospheric Rossby Waves -- 6.5 Atmospheric Blocking Events -- 6.6 Indian Monsoon -- 6.6.1 Paleoclimate Networks -- 6.6.2 Monsoon Extreme Rainfall Events -- 6.7 South American Monsoon -- 6.7.1 Air-Sea Interaction in the South Atlantic Convergence Zone -- 6.7.2 Moisture Sources of Southeastern South America -- 7 Applications to Oceanic Variability -- 7.1 Oceanic El Niño Wave Dynamics -- 7.2 Multidecadal North Atlantic SST Anomalies -- 7.3 Mediterranean Sea Surface Flow Network -- 7.3.1 Network Construction -- 7.3.2 Dispersion and Mixing -- 7.3.3 Communities in the Mediterranean Surface Flow -- 7.4 Optimal Mediterranean Flow Paths -- 8 Climate Tipping Behavior -- 8.1 Climate Tipping Elements -- 8.2 Critical Slowing Down -- 8.3 Atlantic MOC Collapse -- 8.3.1 Models and Data -- 8.3.2 Results for the Two-Dimensional Model -- 8.3.3 Results for the FAMOUS Model -- 8.4 Desertification -- 8.4.1 Vegetation-Water Model -- 8.4.2 Network Approach and Analysis -- 8.5 Percolation-Based Techniques -- 8.5.1 Percolation in the Lorenz'96 Model Network -- 8.5.2 Percolation in Sea Temperature Networks during El Niño Events -- 9 Network-Based Prediction -- 9.1 Concepts of Predictability -- 9.2 Machine Learning -- 9.3 Prediction of the Indian Summer Monsoon -- 9.3.1 The Problem -- 9.3.2 Climate Networks and the Prediction of the Monsoon -- 9.3.3 Prediction of Monsoon Onset and Withdrawal -- 9.3.4 Prediction Skill -- 9.4 El Niño Prediction -- 9.4.1 The Problem -- 9.4.2 Machine Learning Prediction Using Network Measures -- 9.4.3 Prediction Skill -- References -- Copyright Acknowledgments -- Index.
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  • 4
    Keywords: Ocean circulation Mathematical models ; Differentiable dynamical systems ; El Niño Current Mathematical models ; Meeresströmung ; El-Niño-Phänomen
    Type of Medium: Book
    Pages: XVIII, 456 S , graph. Darst., Ill., Kt
    ISBN: 0792365224
    Series Statement: Atmospheric and oceanographic sciences library 22
    DDC: 551.47
    Language: English
    Note: Includes index
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  • 5
    Type of Medium: Book
    Series Statement: Preprints / Koninklijk Nederlands Meteorologisch Instituut 97,30
    Language: Undetermined
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  • 6
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Fluid Mechanics 34 (2002), S. 531-558 
    ISSN: 0066-4189
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: Abstract The El Nino variability in the equatorial Tropical Pacific is characterized by sea-surface temperature anomalies and associated changes in the atmospheric circulation. Through an enormous monitoring effort over the last decades, the relevant time scales and spatial patterns are fairly well documented. In the meantime, a hierarchy of models has been developed to understand the physics of this phenomenon and to make predictions of future variability. In this review, the robust and relevant details of the observations, the fluid mechanical "building blocks," the theory of the deterministic part of the variability, and the impact of small-scale ("noise") and remote ("external") processes are evaluated.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    New York, NY : American Institute of Physics (AIP)
    Physics of Fluids 4 (1992), S. 1915-1928 
    ISSN: 1089-7666
    Source: AIP Digital Archive
    Topics: Physics
    Notes: In this paper the stability of annular pressure-driven parallel flows of two liquids sandwiching a free cylindrical interface is considered. For small to moderate Reynolds numbers, the interface is susceptible to capillary and interfacial wave instabilities, the latter instability caused by a jump in viscosity at the interface. It is shown that favorable velocity profiles in both liquids may stabilize capillary breakup of the interface and suppress the axisymmetric interfacial wave instability. A long-wave analysis leads to the physical mechanism responsible for stabilization of capillary breakup. This physical mechanism is a generalization of that by which capillary breakup is stabilized by interfacial shear in an annular film of a single liquid. Stabilization of intermediate wavelengths is studied with a mechanical energy analysis, which leads to a description of the energetic processes at work.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Physics of Fluids 7 (1995), S. 680-682 
    ISSN: 1089-7666
    Source: AIP Digital Archive
    Topics: Physics
    Notes: Layered double diffusive flow patterns in a laterally heated stably stratified liquid are considered in a configuration which allows for steady states to exist. For the heat/salt system, these flows are characterized by the thermal and solutal Rayleigh numbers RaT and RaS, or equivalently by RaT and the buoyancy ratio Rρ. The bifurcation structure of steady patterns with respect to RaT is computed for two cases: fixed RaS and fixed Rρ. For the first case, results in N. Tsitverblit and E. Kit [Phys. Fluids A 5, 1062 (1993)], are computed and extended, and it is shown that many of the previously found flow patterns are unstable; only in a small interval of RaT, multiple (linearly) stable steady states exist. For the second case, the physical relevance of the unstable steady states with respect to the evolution of the flow toward a stable steady state is demonstrated. © 1995 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    New York, NY : American Institute of Physics (AIP)
    Physics of Fluids 5 (1993), S. 1517-1517 
    ISSN: 1089-7666
    Source: AIP Digital Archive
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Physics of Fluids 9 (1997), S. 615-631 
    ISSN: 1089-7666
    Source: AIP Digital Archive
    Topics: Physics
    Notes: The instability of an arbitrarily shaped zonal jet on a midlatitude β-plane is considered within a two-layer quasi-geostrophic model with O(1) linear friction. Depending on the horizontal and vertical shear of the jet, it is susceptible to both barotropic and baroclinic instabilities. The linear stability boundaries are determined numerically for a parameter regime relevant to the Gulfstream. The weakly nonlinear (finite amplitude) evolution of the instabilities is shown to be governed by a Ginzburg-Landau equation and for arbitrary jet shapes the coefficients in this equation are computed numerically. The finite amplitude state is shown to become unstable to Benjamin-Feir sideband instabilities. The mixed baroclinic/barotropic character of the primary instability is crucial to this sideband instability which is shown to lead to complicated spatio-temporal behavior of the jet. © 1997 American Institute of Physics.
    Type of Medium: Electronic Resource
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