Titlebook: Energy Transfers in Atmosphere and Ocean; Carsten Eden,Armin Iske Book 2019 The Editor(s) (if applicable) and The Author(s), under exclusi

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,Diffuse Interface Approaches in Atmosphere and Ocean—Modeling and Numerical Implementation,tiphase flows with variable densities. We use the . variable density model proposed in Abels et al. (Mathematical Models and Methods in Applied Sciences 22:1150013, .). This results in a Cahn–Hilliard-/Navier–Stokes-type system which we complement with tangential Dirichlet boundary conditions to inc

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The Interior Energy Pathway: Inertia-Gravity Wave Emission by Oceanic Flows,mall Rossby number, e.g., for flows in the vicinity of strong fronts, dissipation occurs in a more complex manner. It can occur via spontaneous wave emission and subsequent wave capture, with the amplitudes of waves emitted in frontal systems being expected to be larger than amplitudes of waves emit

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Observations and Models of Low-Mode Internal Waves in the Ocean,ternal waves is often below unity, and thus, the energy available for mixing must be redistributed by internal tides and near-inertial waves at low vertical wavenumber that can propagate thousands of kilometers from their source regions. Eddy-permitting global ocean circulation models are able to qu

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Diagnosing and Parameterizing the Effects of Oceanic Eddies,rvations and eddying ocean models. A focus will be on Lagrangian particle statistics as an ideal tool to describe the effects of eddies on a time mean transport and to assess the limits and validities of the eddy diffusion model. Eddy diffusivity diagnostics and the current state of eddy parameteriz

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Creating a New Product Concept, goes far beyond conventional gravity wave schemes which are based on the single-column approximation and, in particular, on the strong assumptions of a stationary mean flow and a stationary wave energy equation. The radiative transfer equation has—to our knowledge—never been considered in the atmos

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https://doi.org/10.1007/978-3-031-17354-7ternal waves is often below unity, and thus, the energy available for mixing must be redistributed by internal tides and near-inertial waves at low vertical wavenumber that can propagate thousands of kilometers from their source regions. Eddy-permitting global ocean circulation models are able to qu