{"text_format":"2","workbook":"xls","n_sheets":1,"sheets":["report2"],"not_rendered":{"charts":0,"images":0,"macros":0,"external_links":1,"defined_names":1,"comments":0,"pivot_tables":0},"unopened":[],"bounds":{"document_bytes":16777216,"sheet_cells":100000,"run_cost":"one","rows_first":2000,"rows_last":500,"rows_between":2000,"halvings":0,"cell_chars":16384,"cell_head_chars":4096},"cells_cut":0,"cells_raw":0,"read":"whole","date_system":"1900","formulas":"cached_only"}

{"sheet":"report2","index":0,"n_rows":30,"n_cols":5,"rows_kept":30,"cut":false,"hidden":false,"merged":[[0,2,0,3],[0,4,0,5],[1,2,1,3],[1,4,1,5],[2,2,2,3],[2,4,2,5],[3,2,3,3],[4,2,4,3],[12,2,12,3],[13,2,13,3],[14,2,14,3],[17,2,17,3],[18,2,18,3],[22,2,22,3]],"flags":["formulas_cached_only"]}
[null,"1.","Record Nr.",null,"UNINA9910453250203321"]
[null,null,"Autore",null,"Radko Timour"]
[null,null,"Titolo",null,"Double-diffusive convection / / Timour Radko [[electronic resource]]"]
[null,null,"Pubbl/distr/stampa",null,"Cambridge : , : Cambridge University Press, , 2013"]
[null,null,"ISBN",null,"1-107-28945-9"]
[{"$nulls":4},"1-139-89025-5"]
[{"$nulls":4},"1-107-28901-7"]
[{"$nulls":4},"1-139-03417-0"]
[{"$nulls":4},"1-107-29111-9"]
[{"$nulls":4},"1-107-29390-1"]
[{"$nulls":4},"1-107-29006-6"]
[{"$nulls":4},"1-107-29283-2"]
[null,null,"Descrizione fisica",null,"1 online resource (xv, 342 pages) : digital, PDF file(s)"]
[null,null,"Disciplina",null,"551.46/2"]
[null,null,"Soggetti",null,"Oceanic mixing"]
[{"$nulls":4},"Turbulence"]
[{"$nulls":4},"Salinity"]
[null,null,"Lingua di pubblicazione",null,"Inglese"]
[null,null,"Formato",null,"Materiale a stampa"]
[null,null,null,"Livello bibliografico","Monografia"]
[null,null,null,"Note generali","Title from publisher's bibliographic system (viewed on 05 Oct 2015)."]
[null,null,null,"Nota di bibliografia","Includes bibliographical references and index."]
[null,null,"Nota di contenuto",null,"Cover; Half title; Title; Copyright; Dedication; Contents; Preface; 1 General principles; 1.1 Salt fingers; 1.2 The early years: from Jevons to Stommel; 1.3 Diffusive convection; 1.4 Scale analysis; 1.5 Non-dimensionalization and governing parameters; 1.6 Turner angle; 2 The linear instability problem; 2.1 Conditions for instability; 2.2 Growth rates and spatial scales; 2.3 The flux ratio; 2.4 Effects of horizontal gradients; 3 The unbounded gradient model; 3.1 Flux-gradient laws; 3.2 Secondary instabilities: Stern-Kunze constraint and Holyer modes; 3.3 Weakly nonlinear models"]
[{"$nulls":4},"3.4 Phenomenological and empirical modelsSimilarity solutions; The growth rate balance; Empirical parameterizations; 3.5 Numerical simulations; 3.6 Laboratory experiments; 4 The two-layer system; 4.1 Interfacial flux laws; 4.2 Salt-finger interfaces; 4.3 Diffusive interfaces; 5 The bounded layer model; 5.1 Diffusive layer; 5.2 Salt-finger layer; Planform selection; Vertical transport; Height of the finger zone; 6 Collective instability; 6.1 Approaches; 6.2 Parametric flux-gradient model; 6.3 Physical interpretation; 6.4 Specific solutions; 6.5 Nonlinear "]
[{"$nulls":4},"effects; 7 Thermohaline intrusions"]
[{"$nulls":4},"7.1 Linear theoryPhysical interpretation; The -instability; Preferred scales; Similarity argument; Multiscale model; 7.2 Extensions: rotation, baroclinicity and ambient turbulence; Rotation; Baroclinicity; Ambient turbulence; 7.3 Nonlinear effects; 7.4 Laterally bounded fronts; 7.5 Sidewall heating experiments; 7.6 Oceanographic observations; Success stories; Alternative arguments; Complications; 8 Thermohaline staircases; 8.1 Observations; Salt-finger staircases; Diffusive staircases; 8.2 Staircase origins; Collective instability mechanism; Thermohaline intrusion mechanism"]
[{"$nulls":4},"Metastable equilibria mechanismApplied flux mechanism; Negative density diffusion; 8.3 Instability of the flux-gradient laws; 8.4 Mechanics of layer-merging events; 9 The unified theory of secondary double-diffusive instabilities; 10 Double-diffusion in active environments; 10.1 The interaction of salt fingers with shear flow; 10.2 Low fluxes and thick interfaces; 10.3 The interaction with intermittent turbulence; 10.4 Microstructure signatures of salt fingers in the ocean; Spectral characteristics; Analysis of dissipation measurements; Anisotropy of salt fingers"]
[{"$nulls":4},"10.5 Inverse modeling of thermohaline staircases11 Large-scale consequences; 11.1 Effects of salt fingers; Density stratification and the Meridional Overturning Circulation; The T-S relation and the pattern of density ratio; Regional effects; Biogeochemical applications; Salt fountains in the ocean; 11.2 Effects of diffusive convection; 12 Beyond oceanography; 12.1 Astrophysics; Semiconvection; Fingering convection; 12.2 Geology and geophysics; 12.3 Chemistry; 12.4 Materials science and engineering; Solidification of metal alloys; Solar ponds; 12.5 Other applications"]
[{"$nulls":4},"13 Perspectives and challenges"]
[null,null,null,"Sommario/riassunto","Double-diffusive convection is a mixing process driven by the interaction of two fluid components which diffuse at different rates. Leading expert Timour Radko presents the first systematic overview of the classical theory of double-diffusive convection in a coherent narrative, bringing together the disparate literature in this developing field. The book begins by exploring idealized dynamical models and illustrating key principles by examples of oceanic phenomena. Building on the theory, it then explains the dynamics of structures resulting from double-diffusive instabilities, such as the little-understood phenomenon of thermohaline staircases. The book also surveys non-oceanographic applications, such as industrial, astrophysical and geological manifestations, and discusses the climatic and biological consequences of double-diffusive convection. Providing a balanced blend of fundamental theory and real-world examples, this is an indispensable resource for academic researchers, professionals and graduate students in physical oceanography, fluid dynamics, applied mathematics, astrophysics, geophysics and climatology."]