难管 发表于 2025-3-26 23:54:25
,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描绘 发表于 2025-3-27 04:55:31
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 emitnotion 发表于 2025-3-27 05:33:21
http://reply.papertrans.cn/32/3105/310462/310462_33.png减至最低 发表于 2025-3-27 11:30:08
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 quNarcissist 发表于 2025-3-27 16:34:37
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闯入 发表于 2025-3-27 19:11:08
http://reply.papertrans.cn/32/3105/310462/310462_36.pngTIGER 发表于 2025-3-28 00:21:51
http://reply.papertrans.cn/32/3105/310462/310462_37.pngFLIRT 发表于 2025-3-28 05:46:21
http://reply.papertrans.cn/32/3105/310462/310462_38.png轻快走过 发表于 2025-3-28 09:23:24
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隐士 发表于 2025-3-28 11:45:48
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