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  • 1
    Online Resource
    Online Resource
    New York :Cambridge University Press,
    Keywords: Buoyant convection. ; Electronic books.
    Description / Table of Contents: This book summarizes our present understanding of buoyancy-driven flows, ranging from buoyant coastal currents to dense overflows in the ocean, and from avalanches to volcanic pyroclastic flows. It is an invaluable resource for advanced students and researchers in oceanography, geophysical fluid dynamics, atmospheric science and the wider Earth sciences.
    Type of Medium: Online Resource
    Pages: 1 online resource (446 pages)
    Edition: 1st ed.
    ISBN: 9781139340069
    DDC: 551.48
    Language: English
    Note: Cover -- BUOYANCY-DRIVEN FLOWS -- TITLE -- COPYRIGHT -- Contents -- Contributors -- Introduction -- References -- 1: Gravity Currents - Theory and Laboratory Experiments -- 1.1 Introduction -- 1.2 Reduced Gravity -- 1.3 Frontogenesis -- 1.4 Nondimensional Parameters -- 1.5 Scaling Analysis -- 1.6 Theories for the Froude Number -- 1.6.1 Yih's Theory -- 1.6.2 Von Kármán's Theory -- 1.6.3 Benjamin's Theory -- 1.6.3.1 Mass and Momentum Conservation -- 1.6.3.2 Energy Conservation -- 1.6.3.3 Comparison with Experiment -- 1.6.4 Energy-Conserving Theory -- 1.6.4.1 Partial-Depth Lock Releases -- 1.6.4.2 Mass and Momentum conservation -- 1.6.4.3 Energy Conservation -- 1.6.4.4 Comparison with Experiments -- 1.6.4.5 Energy Transfers -- 1.7 Shallow Water Theory -- 1.7.1 Similarity Solution -- 1.7.1.1 Comparison with Experiment -- 1.8 Stratified Ambient Fluid -- 1.8.1 Criticality -- 1.8.2 Comparison with Data for Stratified Ambient Fluids -- 1.8.2.1 Current Speed -- 1.8.3 Current Depth -- 1.9 Summary and Conclusions -- Acknowledgments -- References -- 2: Theory of Oceanic Buoyancy-Driven Flows -- 2.1 General Considerations and a Laboratory Example -- 2.1.1 Introduction -- 2.1.2 A Laboratory Example: Formulation -- 2.1.3 The Linear Problem -- 2.1.4 The Interior -- 2.1.5 Sidewall Boundary Layers σS < -- < -- 1 -- 2.1.6 The Hydrostatic Layer -- 2.1.7 The Buoyancy Layer -- 2.1.8 Matching the boundary conditions at r = ro -- 2.1.9 The Purely Mechanically Driven Flow -- 2.1.10 The Buoyancy Driven Flow in the Cylinder -- 2.1.11 A Laboratory Example -- 2.2 Buoyancy-Driven Flows in Beta-Plane Basins:The Relation Between Buoyancy Forcing and the Location of Vertical Motion -- 2.2.1 Introduction -- 2.2.2 The Model Formulation -- 2.2.3 Interior Solution -- 2.2.4 Boundary Layer Structure -- 2.2.4.1 The diffusion layer -- 2.2.4.2 The Hydrostatic Layer -- 2.2.5 Matching. , 2.2.6 An Example -- 2.2.7 Nonlinear Theory -- 2.3 Buoyancy Forced Flows with Weak Stratification: Downstream Variation Effects -- 2.3.1 Introduction -- 2.3.2 The Model -- 2.3.3 The Interior -- 2.3.4 The Sidewall Boundary Layer for σH S < -- < -- EH 2/3(D/L)2/3 -- 2.3.5 An Example -- 2.3.6 Discussion -- References -- 3: Buoyancy-Forced Circulation and Downwelling in Marginal Seas -- 3.1 Introduction -- 3.2 Buoyancy-Forced Circulation and Exchange -- 3.2.1 Influence of a Boundary -- 3.2.2 Influence of Sloping Topography -- 3.2.3 Moving Further Toward a More Realistic Configuration -- 3.2.4 Influence of Wind Forcing -- 3.3 Dynamics of Downwelling -- 3.3.1 Dissipative, Stratified Flows -- 3.3.2 Weak Dissipation, Stratified Flows -- 3.3.3 Weakly Stratified Flows -- 3.3.3.1 Along-Channel Evolution -- 3.3.3.2 The Nonhydrostatic Layer -- 3.3.3.3 Cooling Distribution -- 3.3.3.4 Parameter Dependencies -- 3.4 Summary -- Acknowledgments -- References -- 4: Buoyant Coastal Currents -- 4.1 Introduction -- 4.2 A Simple Model for Buoyant Coastal Currents over a Sloping Bottom -- 4.3 Evaluating the Buoyant Coastal Current Model -- 4.3.1 Laboratory model -- 4.3.2 Numerical Model -- 4.3.3 Ocean Observations - The Chesapeake Bay Buoyant Coastal Current -- 4.4 Response of Buoyant Coastal Currents to Wind Forcing -- Acknowledgments -- References -- 5: Overflows and Convectively Driven Flows -- 5.1 Introduction to Overflows -- 5.1.1 What Are Dense Overflows? -- 5.1.2 Denmark Straits Overflow -- 5.1.3 Faroe Bank Channel Overflow -- 5.1.4 Red Sea Overflow -- 5.1.5 Mediterranean Overflow -- 5.1.6 Antarctic Overflows -- 5.1.7 Midocean Ridge Overflows -- 5.1.8 Common Features of Overflows -- 5.2 Overflow Processes: Focus on Entrainment -- 5.2.1 The Entrainment Concept -- 5.2.2 Causes of Entrainment -- 5.2.3 Parameterizing Entrainment -- 5.2.4 Detrainment. , 5.2.5 The Frictional Bottom Boundary Layer -- 5.2.6 Inhomogeneities Across the Overflow Plume -- 5.2.7 Summary -- 5.3 Convectively Driven Ocean Flows -- 5.3.1 Convective Plumes -- 5.3.2 Horizontal Inhomogeneities in Convective Flows -- 5.3.2.1 Localized Buoyancy Forcing -- 5.3.2.2 Convection in the Presence of Lateral Buoyancy Gradients -- 5.3.3 Summary: Contrasting Convection and Overflows -- References -- Appendix: Notation -- 6: An Ocean Climate Modeling Perspective on Buoyancy-Driven Flows -- 6.1 Buoyancy in Ocean Climate Models -- 6.1.1 Reduced Complexity (Box) Models -- 6.1.2 Ocean General Circulation Models for Climate -- 6.1.3 Numerical Constraints and Artifacts -- 6.1.4 Surface Forcing -- 6.1.5 Coupling -- 6.1.6 Concluding remarks on Section 6.1 -- 6.2 Convective Boundary Layers -- 6.2.1 The Ocean Boundary Layer -- 6.2.2 Similarity Theory -- 6.2.3 Penetrative Convection and Spice Injection -- 6.2.4 Concluding Remarks on Section 6.2 -- 6.3 Ventilation in Ocean Models -- 6.3.1 Ideal Age -- 6.3.2 Transit Time Distributions -- 6.3.3 Shallow Ventilation -- 6.3.4 NADW and the AMOC -- 6.3.5 Concluding Remarks on Section 6.3 -- 6.4 Parameterized Overflows -- 6.4.1 Characteristics of Buoyancy-Driven Overflows -- 6.4.2 A Parameterized Mediterranean Overflow -- 6.4.3 Nordic Sea Overflows (Denmark Strait -- Faroe Bank Channel) -- 6.4.4 Comparison with Observations of Ventilation -- 6.4.5 Concluding Remarks on Section 6.4 -- Acknowledgment -- References -- 7: Buoyancy-Driven Currents in Eddying Ocean Models -- 7.1 Introduction -- 7.1.1 Dynamics of Water Mass Formation and Spreading -- 7.1.2 Representing Eddies in Numerical Models: A Historical Perspective -- 7.2 Characteristics of Numerical Models of the Ocean -- 7.3 Interplay of Numerics and Parameterizations -- 7.4 Modeling Deep Flow Through the Romanche Fracture Zone. , 7.5 Modeling the Spreading of Mediterranean Water in the Atlantic -- 7.5.1 The initial descent -- 7.5.2 The Mediterranean undercurrent -- 7.5.3 The Mediterranean Salt Tongue -- 7.6 Conclusion -- List of Acronyms -- References -- 8: Atmospheric Buoyancy-Driven Flows -- 8.1 Introduction -- 8.1.1 The Atmosphere -- 8.1.2 The Weather and the Climate -- 8.1.3 Buoyancy in a Perfect Gas -- 8.2 Circulations -- 8.2.1 Atmospheric Frontal Systems -- 8.2.1.1 The Baroclinic Zone -- 8.2.1.2 Baroclinic Development -- 8.2.1.3 Frontogenesis -- 8.2.2 Atmospheric Convection -- 8.2.2.1 Convective Inhibition and Convective Available Potential Energy -- 8.2.2.2 Downdrafts and Cold Density Currents -- 8.2.2.3 Organization of Convection -- 8.2.3 Direct Cells -- 8.2.3.1 Land/Sea Breeze -- 8.2.3.2 Mountain Breeze -- 8.3 Simulations -- 8.3.1 Overview of Atmospheric Simulations -- 8.3.2 Modeling Buoyancy-Driven Flows -- References -- 9: Volcanic Flows -- 9.1 Introduction -- 9.2 Magma Injection and Eruption Triggering -- 9.3 Second Boiling and Eruption Triggers -- 9.4 Magma Mixing -- 9.4.1 Mixing Prior to Eruption -- 9.4.2 Mixing During Eruption -- 9.5 Eruption Dynamics -- 9.5.1 Eruption Columns -- 9.5.2 Ash Flows -- 9.6 Related Volcanic Processes -- 9.6.1 Submarine Eruptions -- 9.6.2 Hydrothermal Eruptions -- 9.6.3 Lake Nyos Explosion -- 9.7 Summary -- References -- 10: Gravity Flow on Steep Slope -- 10.1 Introduction -- 10.2 A Physical Picture of Gravity Flows -- 10.2.1 Debris Flows -- 10.2.2 Snow Avalanches -- 10.3 Anatomy of Gravity Currents on Slope -- 10.3.1 Anatomy of Debris Flows -- 10.3.2 Anatomy of Powder-Snow Avalanches -- 10.4 Fluid-Mechanics Approach to Gravity Currents -- 10.4.1 Scaling and Flow Regimes -- 10.4.2 Rheology -- 10.4.3 Segregation and Particle Migration -- 10.4.4 Sliding-Block and Box Models -- 10.4.5 Depth-Averaged Equations. , 10.4.6 Asymptotic Expansions -- 10.5 Dense Flows -- 10.5.1 Simple Models -- 10.5.2 Depth-Averaged Equations -- 10.5.3 Elongating Viscoplastic Flows -- 10.6 Dilute Inertia-Dominated Flows -- 10.6.1 Sliding Block Model -- 10.6.2 Depth-Averaged Equations -- 10.7 Comparison with Data -- 10.7.1 Comparison with Laboratory Data -- 10.7.2 Comparison with Field Data -- 10.8 Concluding Remarks and Perspectives -- References -- Index.
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  • 2
    Book
    Book
    New York : Cambridge University Press
    Keywords: Buoyant convection ; Ocean circulation ; Atmospheric circulation ; Strömungsmechanik ; Strömungsmechanik ; Auftrieb ; Fluid ; Auftrieb
    Description / Table of Contents: "This book summarizes present understanding of buoyancy-driven flows for advanced students and researchers in oceanography, geophysical fluid dynamics, atmospheric science, and Earth science"--Provided by publisher
    Type of Medium: Book
    Pages: vii, 436 p., [16] p. of plates , ill. (some col.), maps , 27 cm
    ISBN: 1107008875 , 9781107008878
    DDC: 551.48
    RVK:
    Language: English
    Note: Includes bibliographical references and index , Machine generated contents note: 1. Gravity currents: theory and laboratory Paul Linden; 2. Theory of oceanic buoyancy-driven flows Joseph Pedlosky; 3. Buoyancy-forced circulation and downwelling in marginal seas Michael Spall; 4. Buoyant coastal currents Steve Lentz; 5. Overflows and convectively driven flows Sonya Legg; 6. An ocean climate modeling perspective on buoyancy-driven flows William Large; 7. Buoyancy-driven flows in eddying ocean models Anne Marie Tre;guier, Bruno Ferron, and Raphael Dussin; 8. Atmospheric buoyancy-driven flows Sylvie Malardel; 9. Volcanic flows Andy Woods; 10. Gravity flow on a steep slope Christophe Ancey.
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  • 3
    Publication Date: 2022-05-26
    Description: © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Ocean Modelling 121 (2018): 49-75, doi:10.1016/j.ocemod.2017.11.008.
    Description: Lagrangian analysis is a powerful way to analyse the output of ocean circulation models and other ocean velocity data such as from altimetry. In the Lagrangian approach, large sets of virtual particles are integrated within the three-dimensional, time-evolving velocity fields. Over several decades, a variety of tools and methods for this purpose have emerged. Here, we review the state of the art in the field of Lagrangian analysis of ocean velocity data, starting from a fundamental kinematic framework and with a focus on large-scale open ocean applications. Beyond the use of explicit velocity fields, we consider the influence of unresolved physics and dynamics on particle trajectories. We comprehensively list and discuss the tools currently available for tracking virtual particles. We then showcase some of the innovative applications of trajectory data, and conclude with some open questions and an outlook. The overall goal of this review paper is to reconcile some of the different techniques and methods in Lagrangian ocean analysis, while recognising the rich diversity of codes that have and continue to emerge, and the challenges of the coming age of petascale computing.
    Description: EvS has received funding from the European Research Council (ERC) under the European Unions Horizon 2020 research and innovation programme (grant agreement No 715386). This research for PJW was supported as part of the Energy Exascale Earth System Model (E3SM) project, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research. Funding for HFD was provided by Grant No. DE-SC0012457 from the US Department of Energy. PB acknowledges support for this work from NERC grant NE/R011567/1. SFG is supported by NERC National Capability funding through the Extended Ellett Line Programme.
    Keywords: Ocean circulation ; Lagrangian analysis ; Connectivity ; Particle tracking ; Future modelling
    Repository Name: Woods Hole Open Access Server
    Type: Article
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