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Oceanography --- Mathematical models. --- Mathematical models --- Oceanography - Mathematical models. --- Modélisation --- Traitement des donnees --- Hydrodynamique --- Modeles mathematiques --- Hydrodynamique -- Modeles mathematiques
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Marine Forecasting
Colloques --- Colloquia --- Mechanica --- Mécanique --- Oceanografie --- Océanographie --- Oceanography --- Hydrodynamics --- Mathematical models --- Congresses --- Congresses. --- Issue --- Conferences - Meetings --- Oceanography, Physical --- Oceanology --- Physical oceanography --- Thalassography --- Earth sciences --- Marine sciences --- Ocean --- Fluid dynamics --- Mathematical models&delete& --- Oceanography - Mathematical models - Congresses --- Hydrodynamics - Mathematical models - Congresses
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Larry Pratt received his Ph. D. in physical oceanography in the Woods Hole/MIT Joint Program in 1982. He then served as a research associate and assistant research professor at the University of Rhode Island before joining the scientific staff at the Woods Hole Oceanographic Institution, where he is now a senior scientist. He is editor of The Physical Oceanography of Sea Straits and has authored or co-authored numerous articles on hydraulic effects in the ocean. J. A. (Jack) Whitehead received his Ph. D. in engineering and applied science from Yale University in 1968. After postdoctoral work and serving as assistant research geophysicist at the Institute of Geophysical and Planetary Physics at UCLA, he joined the scientific staff at the Woods Hole Oceanographic Institution, where he is now a Senior Scientist. He has authored or co-authored numerous articles on hydraulic effects in the ocean. Hydraulic effects can occur when high-speed ocean currents and atmospheric winds encounter strong topographic features. This book contains a deep and extensive discussion of geophysical flows that are broad enough to be influenced by Earth's rotation and strong enough to experience classical hydraulic effects such as critical control and hydraulic jumps. Examples include deep overflows and coastal currents in the ocean and winds in the coastal marine layer. The material is appropriate for students at the graduate or advanced undergraduate level who have some elementary knowledge of fluid mechanics. Reviews of geophysical observations and of the hydraulics of flow with no background rotation are followed by chapters on models of currents in rotating channels, shock waves and time dependence, coastal flow, two-layer stratification, and jets. Although the primary focus is on the theory, a number of case studies, including the Faroe Bank overflow and the California coastal marine layer winds, are presented along with numerous laboratory experiments. Exercises are presented at the end of most sections. The presentation should allow the reader to develop a thorough understanding of the fundamentals of the hydraulics of rotating flows.
Electronic books. -- local. --- Hydrodynamics. --- Rotating masses of fluid. --- Rotating masses of fluid --- Water masses --- Hydrodynamics --- Oceanography --- Applied Mathematics --- Marine Science --- Engineering & Applied Sciences --- Earth & Environmental Sciences --- Mathematical models --- Hydrodynamics - Mathematical models --- Oceanography - Mathematical models
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Oceans play a pivotal role in our weather and climate. Ocean-borne commerce is vital to our increasingly close-knit global community. Yet we do not fully understand the intricate details of how they function, how they interact with the atmosphere, and what the limits are to their biological productivity and their tolerance to wastes. While satellites are helping us to fill in the gaps, numerical ocean models are playing an important role in increasing our ability to comprehend oceanic processes, monitor the current state of the oceans, and to a limited extent, even predict their future state.
Oceanography --- Mathematical models. --- Geografie --- Topografie --- Hydrografie. --- Mathematical models --- Earth Sciences --- General and Others --- Oceanography, Physical --- Oceanology --- Physical oceanography --- Thalassography --- Earth sciences --- Marine sciences --- Ocean --- Computer simulation. --- Oceanography - Mathematical models
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Inverse Modeling of the Ocean and Atmosphere is a graduate-level book for students of oceanography and meteorology, and anyone interested in combining computer models and observations of the hydrosphere or solid earth. A step-by-step development of maximally efficient inversion algorithms, using ideal models, is complemented by computer codes and comprehensive details for realistic models. Variational tools and statistical concepts are concisely introduced, and applications to contemporary research models, together with elaborate observing systems, are examined in detail. The book offers a review of the various alternative approaches, and further advanced research topics are discussed. Derived from the author's lecture notes, this book constitutes an ideal course companion for graduate students, as well as being a valuable reference source for researchers and managers in theoretical earth science, civil engineering and applied mathematics.
Oceanography --- Meteorology --- Inverse problems (Differential equations) --- Differential equations --- Mathematical models. --- Mathematical models --- Océanographie --- Météorologie --- Problèmes inversés (Equations différentielles) --- Modèles mathématiques --- Oceanography - Mathematical models --- Meteorology - Mathematical models
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Offers an introduction to computer-based modelling of oceanic processes. This title contains over twenty practical exercises, using freely available Open-Source software, and covers a range of topics from long surface waves, geostrophic flows, through to the general wind-driven circulation including western boundary currents and mesoscale eddies.
Meereskunde -- Numerisches Modell. --- Meereskunde. --- Numerisches Modell. --- Oceanography -- Computer simulation. --- Oceanography -- Mathematical models. --- Oceanography --- Marine Science --- Earth & Environmental Sciences --- Computer simulation --- Mathematical models --- Computer programs. --- Mathematical models. --- Earth sciences. --- Climatology. --- Geophysics. --- Oceanography. --- Fluids. --- Earth Sciences. --- Geophysics and Environmental Physics. --- Fluid- and Aerodynamics. --- Geophysics/Geodesy. --- Physical geography. --- Geography --- Oceanography, Physical --- Oceanology --- Physical oceanography --- Thalassography --- Earth sciences --- Marine sciences --- Ocean --- Hydraulics --- Mechanics --- Physics --- Hydrostatics --- Permeability --- Climate --- Climate science --- Climate sciences --- Science of climate --- Atmospheric science --- Geological physics --- Terrestrial physics --- Oceanography - Computer simulation --- Oceanography - Mathematical models
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The realism of large scale numerical ocean models has improved dra matically in recent years, in part because modern computers permit a more faithful representation of the differential equations by their algebraic analogs. Equally significant, if not more so, has been the improved under standing of physical processes on space and time scales smaller than those that can be represented in such models. Today, some of the most challeng ing issues remaining in ocean modeling are associated with parameterizing the effects of these high-frequency, small-space scale processes. Accurate parameterizations are especially needed in long term integrations of coarse resolution ocean models that are designed to understand the ocean vari ability within the climate system on seasonal to decadal time scales. Traditionally, parameterizations of subgrid-scale, high-frequency mo tions in ocean modeling have been based on simple formulations, such as the Reynolds decomposition with constant diffusivity values. Until recently, modelers were concerned with first order issues such as a correct represen tation of the basic features of the ocean circulation. As the numerical simu lations become better and less dependent on the discretization choices, the focus is turning to the physics of the needed parameterizations and their numerical implementation. At the present time, the success of any large scale numerical simulation is directly dependent upon the choices that are made for the parameterization of various subgrid processes.
Oceanography --- Mathematical models --- Oceanography. --- Mathematical physics. --- Continuum physics. --- Theoretical, Mathematical and Computational Physics. --- Classical and Continuum Physics. --- Classical field theory --- Continuum physics --- Physics --- Continuum mechanics --- Physical mathematics --- Oceanography, Physical --- Oceanology --- Physical oceanography --- Thalassography --- Earth sciences --- Marine sciences --- Ocean --- Mathematics --- Oceanography - Mathematical models
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'Ocean Biogeochemical Dynamics' provides a broad theoretical framework upon which graduate students and upper-level undergraduates can formulate an understanding of the processes that control the mean concentration and distribution of biologically utilized elements and compounds in the ocean. Though it is written as a textbook, it will also be of interest to more advanced scientists as a wide-ranging synthesis of our present understanding of ocean biogeochemical processes. The first two chapters of the book provide an introductory overview of biogeochemical and physical oceanography. The next four chapters concentrate on processes at the air-sea interface, the production of organic matter in the upper ocean, the remineralization of organic matter in the water column, and the processing of organic matter in the sediments. The focus of these chapters is on analyzing the cycles of organic carbon, oxygen, and nutrients. The next three chapters round out the authors' coverage of ocean biogeochemical cycles with discussions of silica, dissolved inorganic carbon and alkalinity, and CaCO3. The final chapter discusses applications of ocean biogeochemistry to our understanding of the role of the ocean carbon cycle in interannual to decadal variability, paleoclimatology, and the anthropogenic carbon budget. The problem sets included at the end of each chapter encourage students to ask critical questions in this exciting new field. While much of the approach is mathematical, the math is at a level that should be accessible to students with a year or two of college level mathematics and/or physics.
Chemical oceanography --- Biogeochemistry --- Océanographie chimique --- Biogéochimie --- Mathematical models --- Biogeochemistry. --- Chemical oceanography. --- Mathematical models. --- Océanographie chimique --- Biogéochimie --- Marine chemistry --- Océanographie chimique. --- Biogéochimie. --- Modèles mathématiques --- Modèles mathématiques. --- Oceanography --- Water chemistry --- Biochemistry --- Geochemistry --- Chemical oceanography - Mathematical models --- Biogeochemistry - Mathematical models --- Océanographie chimique. --- Biogéochimie. --- Modèles mathématiques.
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Numerical Modelling of Marine Hydrodynamics
Oceanography --- Hydrodynamics --- Mathematical models --- -Oceanography --- -532 --- Oceanography, Physical --- Oceanology --- Physical oceanography --- Thalassography --- Earth sciences --- Marine sciences --- Ocean --- Fluid dynamics --- Fluid mechanics in general. Mechanics of liquids (hydromechanics) --- Mathematical models. --- 532 Fluid mechanics in general. Mechanics of liquids (hydromechanics) --- 532 --- Oceanography - Mathematical models --- Hydrodynamics - Mathematical models
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