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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Oceanography. ; Electronic books.
    Description / Table of Contents: Proceedings of the NATO Advanced Study Institute, Les Houches, France, January 20-30, 1998.
    Type of Medium: Online Resource
    Pages: 1 online resource (459 pages)
    Edition: 1st ed.
    ISBN: 9789401150965
    Series Statement: Nato Science Series C: Series ; v.516
    DDC: 551.4/6/0015/118
    Language: English
    Note: Intro -- TABLE OF CONTENTS -- PREFACE.
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  • 2
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Oceanography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (586 pages)
    Edition: 1st ed.
    ISBN: 9781402040283
    Language: English
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  • 3
    Keywords: Konferenzschrift ; Meer ; Meereskunde ; Mathematisches Modell ; Angewandte Mathematik
    Description / Table of Contents: Aus dem Inhalt: Preface. 1) Oceanic general circulation models 2) Forcing the ocean 3) Modeling and parameterizing the ocean planetary boundary layer 4) Parameterization of the fair weather Ekman layer 5) The representation of bottom boundary layer processes in numerical ocean circulation models 6) Marginal sea overflows for climate simulations 7) Turbulent mixing in the ocean: Intensity, causes, and consequences 8) Parameterization of processes in deep convection regimes 9) Double-diffusive convection: its role in ocean mixing and parameterization schemes for large scale modeling 10) Interleaving at the equator: its parameterization and effect on the large scale dynamics 11) Eddy parameterization in large scale flow 12) Three-dimensional residual-mean theory 13) Statistical mechanics of potential vorticity for parameterizing mesoscale eddies . 14) Topographic stress: importance and parameterization 15) Large-eddy simulations of three-dimensional turbulent flows: geophysical applications 16) Parameter estimation in dynamical models 17) On the large-scale modeling of sea ice and sea ice-ocean interactions 18) Ocean modeling in isopycnic coordinates
    Type of Medium: Book
    Pages: VIII, 451 S , graph. Darst.
    ISBN: 0792352289
    Series Statement: NATO science series 516
    Language: English
    Note: Published in cooperation with NATO Scientific Affairs Division , Includes index
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  • 4
    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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  • 5
    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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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 12 (1995), S. 53-65 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Spatial patterns of mid-latitude large-scale ocean-atmosphere interaction on monthly to seasonal time scales have been observed to exhibit a similar structure in both the North Pacific and North Atlantic basins. These patterns have been interpreted as a generic oceanic response to surface wind anomalies, whereby the anomalous winds give rise to corresponding anomalous regions of surface heat flux and consequent oceanic cooling. This mechanistic concept is investigated in this study using numerical models of a global atmosphere and a mid-latitude ocean basin (nominally the Atlantic). The models were run in both coupled and uncoupled mode. Model output was used to generate multi-year time series of monthly mean fields. Empirical orthogonal function (EOF) and singular value decomposition (SVD) analyses were then used to obtain the principal patterns of variability in heat flux, air temperature, wind speed, and sea surface temperature (SST), and to determine the relationships among these variables. SVD analysis indicates that the turbulent heat flux from the ocean to the atmosphere is primarily controlled by the surface scalar wind speed, and to a lesser extent by air temperature and SST. The principal patterns of air-sea interaction are closely analogous to those found in observational data. In the atmosphere, the pattern consists of a simultaneous strengthening (or weakening) of the mid-latitude westerlies and the easterly trades. In the ocean there is cooling (warming) under the anomalously strong (weak) westerlies and trade winds, with a weaker warming (cooling) in the region separating the westerly and easterly wind regimes. These patterns occur in both coupled and uncoupled models and the primary influence of the coupling is in localizing the interaction patterns. The oceanic patterns can be explained by the principal patterns of surface heat flux and the attendant warming or cooling of the ocean mixed layer.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 12 (1995), S. 53-65 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract. Spatial patterns of mid-latitude large-scale ocean-atmosphere interaction on monthly to seasonal time scales have been observed to exhibit a similar structure in both the North Pacific and North Atlantic basins. These patterns have been interpreted as a generic oceanic response to surface wind anomalies, whereby the anomalous winds give rise to corresponding anomalous regions of surface heat flux and consequent oceanic cooling. This mechanistic concept is investigated in this study using numerical models of a global atmosphere and a mid-latitude ocean basin (nominally the Atlantic). The models were run in both coupled and uncoupled mode. Model output was used to generate multi-year time series of monthly mean fields. Empirical orthogonal function (EOF) and singular value decomposition (SVD) analyses were then used to obtain the principal patterns of variability in heat flux, air temperature, wind speed, and sea surface temperature (SST), and to determine the relationships among these variables. SVD analysis indicates that the turbulent heat flux from the ocean to the atmosphere is primarily controlled by the surface scalar wind speed, and to a lesser extent by air temperature and SST. The principal patterns of air-sea interaction are closely analogous to those found in observational data. In the atmosphere, the pattern consists of a simultaneous strengthening (or weakening) of the mid-latitude westerlies and the easterly trades. In the ocean there is cooling (warming) under the anomalously strong (weak) westerlies and trade winds, with a weaker warming (cooling) in the region separating the westerly and easterly wind regimes. These patterns occur in both coupled and uncoupled models and the primary influence of the coupling is in localizing the interaction patterns. The oceanic patterns can be explained by the principal patterns of surface heat flux and the attendant warming or cooling of the ocean mixed layer.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2021-02-08
    Description: Highlights: • Lagrangian ocean analysis is a powerful way to analyse the output of ocean circulation models • We present a review of the Kinematic framework, available tools, and applications of Lagrangian ocean analysis • While there are unresolved questions, the framework is robust enough to be used widely in ocean modelling Abstract: 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.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2021-02-08
    Description: We present a new surface-atmospheric dataset for driving ocean–sea-ice models based on Japanese 55-year atmospheric reanalysis (JRA-55), referred to here as JRA55-do. The JRA55-do dataset aims to replace the CORE interannual forcing version 2 (hereafter called the CORE dataset), which is currently used in the framework of the Coordinated Ocean-ice Reference Experiments (COREs) and the Ocean Model Intercomparison Project (OMIP). A major improvement in JRA55-do is the refined horizontal grid spacing (∼ 55 km) and temporal interval (3 hr). The data production method for JRA55-do essentially follows that of the CORE dataset, whereby the surface fields from an atmospheric reanalysis are adjusted relative to reference datasets. To improve the adjustment method, we use high-quality products derived from satellites and from several other atmospheric reanalysis projects, as well as feedback on the CORE dataset from the ocean modelling community. Notably, the surface air temperature and specific humidity are adjusted using multi-reanalysis ensemble means. In JRA55-do, the downwelling radiative fluxes and precipitation, which are affected by an ambiguous cloud parameterisation employed in the atmospheric model used for the reanalysis, are based on the reanalysis products. This approach represents a notable change from the CORE dataset, which imported independent observational products. Consequently, the JRA55-do dataset is more self-contained than the CORE dataset, and thus can be continually updated in near real-time. The JRA55-do dataset extends from 1958 to the present, with updates expected at least annually. This paper details the adjustments to the original JRA-55 fields, the scientific rationale for these adjustments, and the evaluation of JRA55-do. The adjustments successfully corrected the biases in the original JRA-55 fields. The globally averaged features are similar between the JRA55-do and CORE datasets, implying that JRA55-do can suitably replace the CORE dataset for use in driving global ocean–sea-ice models.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2019-02-01
    Description: The Ocean Model Intercomparison Project (OMIP) is an endorsed project in the Coupled Model Intercomparison Project Phase 6 (CMIP6). OMIP addresses CMIP6 science questions, investigating the origins and consequences of systematic model biases. It does so by providing a framework for evaluating (including assessment of systematic biases), understanding, and improving ocean, sea-ice, tracer, and biogeochemical components of climate and earth system models contributing to CMIP6. Among the WCRP Grand Challenges in climate science (GCs), OMIP primarily contributes to the regional sea level change and near-term (climate/decadal) prediction GCs. OMIP provides (a) an experimental protocol for global ocean/sea-ice models run with a prescribed atmospheric forcing; and (b) a protocol for ocean diagnostics to be saved as part of CMIP6. We focus here on the physical component of OMIP, with a companion paper (Orr et al., 2016) detailing methods for the inert chemistry and interactive biogeochemistry. The physical portion of the OMIP experimental protocol follows the interannual Coordinated Ocean-ice Reference Experiments (CORE-II). Since 2009, CORE-I (Normal Year Forcing) and CORE-II (Interannual Forcing) have become the standard methods to evaluate global ocean/sea-ice simulations and to examine mechanisms for forced ocean climate variability. The OMIP diagnostic protocol is relevant for any ocean model component of CMIP6, including the DECK (Diagnostic, Evaluation and Characterization of Klima experiments), historical simulations, FAFMIP (Flux Anomaly Forced MIP), C4MIP (Coupled Carbon Cycle Climate MIP), DAMIP (Detection and Attribution MIP), DCPP (Decadal Climate Prediction Project), ScenarioMIP, HighResMIP (High Resolution MIP), as well as the ocean/sea-ice OMIP simulations
    Type: Article , PeerReviewed
    Format: text
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