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  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Oceanography--Mathematical models. ; Electronic books.
    Description / Table of Contents: Addressing the problems of making inferences from noisy observations and imperfect theories, this 2006 book introduces many inference tools and practical applications. Starting with fundamental algebraic and statistical ideas, it is ideal for graduate students and researchers in oceanography, climate science, and geophysical fluid dynamics.
    Type of Medium: Online Resource
    Pages: 1 online resource (397 pages)
    Edition: 1st ed.
    ISBN: 9780511219276
    DDC: 551.4601519287
    Language: English
    Note: Cover -- Half-title -- Title -- Copyright -- Dedication -- Contents -- Preface -- Acknowledgements -- Part I Fundamental machinery -- 1 Introduction -- 1.1 Differential equations -- 1.2 Partial differential equations -- 1.3 More examples -- A tracer box model -- A tomographic problem -- A second tracer problem -- Vibrating string -- 1.4 Importance of the forward model -- Notes -- 2 Basic machinery -- 2.1 Background -- 2.2 Matrix and vector algebra -- Matrices and vectors -- Gram-Schmidt process -- 2.2.1 Matrix multiplication and identities -- 2.2.2 Linear simultaneous equations -- 2.2.3 Matrix norms -- 2.2.4 Identities: differentiation -- 2.3 Simple statistics: regression -- 2.3.1 Probability densities, moments -- 2.3.2 Sample estimates: bias -- 2.3.3 Functions and sums of random variables -- 2.3.4 Multivariable probability densities: correlation -- 2.3.5 Change of variables -- Vector random processes -- 2.3.6 Sums of random variables -- Degrees-of-Freedom -- Stationarity -- 2.4 Least-squares -- 2.4.1 Basic formulation -- 2.4.2 Weighted and tapered least-squares -- 2.4.3 Underdetermined systems and Lagrange multipliers -- Lagrange multipliers and adjoints -- 2.4.4 Interpretation of discrete adjoints -- 2.5 The singular vector expansion -- 2.5.1 Simple vector expansions -- 2.5.2 Square-symmetric problem: eigenvalues/eigenvectors -- 2.5.3 Arbitrary systems -- The singular vector expansion and singular value decomposition -- 2.5.4 The singular value decomposition -- 2.5.5 Some simple examples: algebraic equations -- 2.5.6 Simple examples: differential and partial differential equations -- 2.5.7 Relation of least-squares to the SVD -- 2.5.8 Pseudo-inverses -- 2.5.9 Row and column scaling -- Column scaling -- 2.5.10 Solution and observation resolution: data ranking -- 2.5.11 Relation to tapered and weighted least-squares. , 2.5.12 Resolution and variance of tapered solutions -- 2.6 Combined least-squares and adjoints -- 2.6.1 Exact constraints -- 2.6.2 Relation to Green functions -- 2.7 Minimum variance estimation and simultaneous equations -- 2.7.1 The fundamental result -- 2.7.2 Linear algebraic equations -- 2.7.3 Testing after the fact -- 2.7.4 Use of basis functions -- 2.7.5 Determining a mean value -- 2.8 Improving recursively -- 2.8.1 Least-squares -- 2.8.2 Minimum variance recursive estimates -- 2.9 Summary -- Appendix 1. Maximum likelihood -- Appendix 2. Differential operators and Green functions -- Appendix 3. Recursive least-squares and Gauss-Markov solutions -- Notes -- 3 Extensions of methods -- 3.1 The general eigenvector/eigenvalue problem -- 3.2 Sampling -- 3.2.1 One-dimensional interpolation -- 3.2.2 Higher-dimensional mapping -- 3.2.3 Mapping derivatives -- 3.3 Inequality constraints: non-negative least-squares -- 3.4 Linear programming -- 3.5 Empirical orthogonal functions -- 3.6 Kriging and other variants of Gauss-Markov estimation -- 3.7 Non-linear problems -- 3.7.1 Total least-squares -- 3.7.2 Method of total inversion -- 3.7.3 Variant non-linear methods, including combinatorial ones -- Notes -- 4 The time-dependent inverse problem: state estimation -- 4.1 Background -- 4.2 Basic ideas and notation -- 4.2.1 Models -- 4.2.2 How to find the matrix A(t) -- 4.2.3 Observations and data -- 4.3 Estimation -- 4.3.1 Model and data consistency -- 4.3.2 The Kalman filter -- 4.3.3 The smoothing problem -- 4.3.4 Other smoothers -- 4.4 Control and estimation problems -- 4.4.1 Lagrange multipliers and adjoints -- 4.4.2 Terminal constraint problem: open-loop control -- 4.4.3 Representers and boundary Green functions -- 4.4.4 The control Riccati equation -- 4.4.5 The initialization problem -- 4.5 Duality and simplification: the steady-state filter and adjoint. , 4.6 Controllability and observability -- Controllability -- Observability -- 4.7 Non-linear models -- 4.7.1 The linearized and extended Kalman filter -- 4.7.2 Parameter estimation and adaptive estimation -- 4.7.3 Non-linear adjoint equations: searching for solutions -- 4.7.4 Automatic differentiation, linearization, and sensitivity -- 4.7.5 Approximate methods -- 4.8 Forward models -- 4.9 A summary -- Appendix. Automatic differentiation and adjoints -- Notes -- 5 Time-dependent methods - 2 -- 5.1 Monte Carlo/ensemble methods -- 5.1.1 Ensemble methods and particle filters -- 5.2 Numerical engineering: the search for practicality -- 5.2.1 Meteorological assimilation -- 5.2.2 Nudging and objective mapping -- 5.2.3 Approximate filter/smoother methods -- Steady-state approximation -- 5.2.4 Reduced state methods -- Other approaches to state reduction -- 5.3 Uncertainty in Lagrange multiplier method -- 5.4 Non-normal systems -- 5.4.1 POPs and optimal modes -- 5.5 Adaptive problems -- Appendix. Doubling -- Notes -- Part II Applications -- 6 Applications to steady problems -- 6.1 Steady-state tracer distributions -- 6.2 The steady ocean circulation inverse problem -- 6.2.1 Equations of motion -- 6.2.2 Geostrophy -- The classical dynamic method -- 6.2.3 Integral version -- 6.2.4 Discrete version -- 6.2.5 A specific example -- 6.2.6 Solution by SVD -- Controlling the solution -- 6.2.7 Solution by Gauss-Markov estimate -- 6.2.8 Adding further properties -- 6.3 Property fluxes -- 6.4 Application to real oceanographic problems -- 6.4.1 Regional applications -- 6.4.2 The columnar result -- 6.4.3 Global-scale applications -- 6.4.4 Error estimates -- 6.4.5 Finite-difference models -- 6.5 Linear programming solutions -- 6.6 The β-spiral and variant methods -- 6.6.1 The β-spiral -- 6.7 Alleged failure of inverse methods. , 6.8 Applications of empirical orthogonal functions (EOFs) (singular vectors) -- 6.9 Non-linear problems -- Notes -- 7 Applications to time-dependent fluid problems -- 7.1 Time-dependent tracers -- 7.2 Global ocean states by Lagrange multiplier methods -- 7.3 Global ocean states by sequential methods -- 7.4 Miscellaneous approximations and applications -- 7.5 Meteorological applications -- References -- Index.
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  • 2
    Keywords: Stommel, Henry M ; Oceanography
    Type of Medium: Book
    Pages: XXXIII, 623 S. , Ill., graph. Darst., Kt. , 1 Beil.
    ISBN: 0262231042
    DDC: 551.46
    Language: English
    Note: Bibliography: p. 554-611 , Includes index
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  • 3
    Book
    Book
    Cambridge [u.a.] : Cambridge University Press
    Keywords: Ocean tomography ; Jugend ; Jugend ; Hydroakustik
    Type of Medium: Book
    Pages: 433 S.
    Edition: 1.publ.
    ISBN: 0521470951
    Series Statement: Cambridge monographs on mechanics
    DDC: 620.2/5
    RVK:
    Language: English
    Note: Includes bibliographical references and index
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  • 4
    Book
    Book
    Princeton, New Jersey : Princeton University Press
    Keywords: Oceanography ; Oceanography Observations ; Meereskunde ; Meereskunde
    Description / Table of Contents: "With the advent of computers, novel instruments, satellite technology, and increasingly powerful modeling tools, we know more about the ocean than ever before. Yet we also have a new generation of oceanographers who have become increasingly distanced from the object of their study. Ever-fewer scientists collect the observational data on which they base their research. Instead, many download information without always fully understanding how far removed it is from the original data, with opportunity for great misinterpretation. This textbook introduces modern physical oceanography to beginning graduate students and experienced practitioners in allied fields. Real observations are strongly emphasized, as is their implications for understanding the behavior of the global ocean. Written by a leading physical oceanographer, Physical Oceanography and the Oceanic General Circulation explains what the observational revolution of the past twenty-five years has taught us about the real, changing fluid ocean. Unlike any existing book, it provides a comprehensive and accessible treatment of the subject, covering everything from modern methods of observation and data analysis to the fluid dynamics and modeling of ocean processes and variability. Fully illustrated in color throughout, the book describes the fundamental concepts that are needed before delving into more advanced topics, including internal-inertial waves, tides, balanced motions, and large-scale circulation physics"--
    Type of Medium: Book
    Pages: xv, 493 Seiten , Illustrationen, Diagramme , 26 cm
    ISBN: 0691158827 , 9780691158822
    DDC: 551.46
    RVK:
    Language: English
    Note: Literaturverzeichnis: Seiten [447]-476
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  • 5
    In: Journal of fluid mechanics ; 53.1972
    Type of Medium: Book
    Pages: S. 17 - 44 , graph. Darst
    Series Statement: Technical report / Woods Hole Oceanographic Institution 72-58
    Language: English
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  • 6
    Book
    Book
    Cambridge : Cambridge University Press
    Keywords: Ocean circulation Mathematical models ; Inverse problems (Differential equations) ; Meer ; Zirkulation ; Meeresströmung ; Mathematisches Modell ; Inverses Problem ; Differentialgleichung ; Meer ; Zirkulation ; Meeresströmung ; Mathematisches Modell ; Inverses Problem ; Differentialgleichung ; Meeresströmung ; Mathematisches Modell
    Type of Medium: Book
    Pages: XIV, 442 S. , Ill., Kt.
    ISBN: 0521480906
    RVK:
    Language: English
    Note: Includes bibliographical references and indexes
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  • 7
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Fluid Mechanics 36 (2004), S. 281-314 
    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: The coexistence in the deep ocean of a finite, stable stratification, a strong meridional overturning circulation, and mesoscale eddies raises complex questions concerning the circulation energetics. In particular, small-scale mixing processes are necessary to resupply the potential energy removed in the interior by the overturning and eddy-generating process. A number of lines of evidence, none complete, suggest that the oceanic general circulation, far from being a heat engine, is almost wholly governed by the forcing of the wind field and secondarily by deep water tides. In detail however, the budget of mechanical energy input into the ocean is poorly constrained. The now inescapable conclusion that over most of the ocean significant "vertical" mixing is confined to topographically complex boundary areas implies a potentially radically different interior circulation than is possible with uniform mixing. Whether ocean circulation models, either simple box or full numerical ones, neither explicitly accounting for the energy input into the system nor providing for spatial variability in the mixing, have any physical relevance under changed climate conditions is at issue.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 26 (1998), S. 219-253 
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Notes: Abstract For technical reasons, the general circulation of the ocean has historically been treated as a steady, laminar flow field. The recent availability of extremely high-accuracy and high-precision satellite altimetry has provided a graphic demonstration that the ocean is actually a rapidly time-evolving turbulent flow field. To render the observations quantitatively useful for oceanographic purposes has required order of magnitude improvements in a number of fields, including orbit dynamics, gravity field estimation, and atmospheric variability. With five years of very high-quality data now available, the nature of oceanic variability on all space and time scales is emerging, including new findings about such diverse and important phenomena as mixing coefficients, the frequency/wavenumber spectrum, and turbulent cascades. Because the surface elevation is both a cause and consequence of motions deep within the water column, oceanographers soon will be able to provide general circulation numerical models tested against and then combined with the altimeter data. These will be complete three-dimensional time-evolving estimates of the ocean circulation, permitting greatly improved estimates of oceanic heat, carbon, and other property fluxes.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 307 (1984), S. 447-450 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] To make a direct comparison of temperature in the two investigations, we have interpolated the data to common locations (excluding segments at the ends where the lines did not coincide). A fine mesh was generated (grid points over 40m vertically and every 10 km horizontally) using the technique of ...
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 271 (1978), S. 286-286 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] THIS monograph by three well-known Soviet oceanographers is a survey of the physical variability of the oceans on widely varying space and timescales. Although the writing is clear and the errors few, I suspect that the book will have a limited readership. The major shortcoming is that the most ...
    Type of Medium: Electronic Resource
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