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Energy Transfers in Atmosphere and Ocean

Part of the Mathematics of Planet Earth Book Series (volume 1)

Editors: Eden, Carsten; Iske, Armin

DOI: 10.1007/978-3-030-05704-6

ISBN: 978-3-030-05703-9

Publisher: Springer International Publishing - Springer Journals

Jan 24, 2019

1 - 9 of 9 Chapters

LitStream

Chapter 1Multi-scale Methods for Geophysical Flows

Franzke, Christian L. E.; Oliver, Marcel; Rademacher, Jens D. M.; Badin, Gualtiero

Pages: 1 –51

[Geophysical flows comprise a broad range of spatial and temporal scales, from planetary- to meso-scale and microscopic turbulence regimes. The relation of scales and flow phenomena is essential in order to validate and improve current numerical weather and climate prediction models. While regime...
LitStream

Chapter 2The Interior Energy Pathway: Inertia-Gravity Wave Emission by Oceanic Flows

von Storch, Jin-Song; Badin, Gualtiero; Oliver, Marcel

Pages: 53 –85

[We review the possible role of spontaneous emission and subsequent capture of internal gravity waves (IGWs) for dissipation in oceanic flows under conditions characteristic for the ocean circulation. Dissipation is necessary for the transfer of energy from the essentially balanced large-scale...
LitStream

Chapter 3The IDEMIX Model: Parameterization of Internal Gravity Waves for Circulation Models of Ocean and Atmosphere

Olbers, Dirk; Eden, Carsten; Becker, Erich; Pollmann, Friederike; Jungclaus, Johann

Pages: 87 –125

[The IDEMIX conceptIDEMIXconcept is an energetically consistent framework to describe wave effects in circulation models of ocean and atmosphere. It is based on the radiative transfer equation for an internal gravity wave field in physical and wavenumber space and was shown to be successful for...
LitStream

Chapter 4Observations and Models of Low-Mode Internal Waves in the Ocean

Mertens, Christian; Köhler, Janna; Walter, Maren; von Storch, Jin-Song; Rhein, Monika

Pages: 127 –143

[The generation of internal gravity waves in the ocean is largely driven by tides, winds, and interaction of currents with the seafloor. Models and observations indicate a global energy supply for the internal wave field of about 1 TW by the conversion of barotropic tides at mid-ocean ridges and...
LitStream

Chapter 5Toward Consistent Subgrid Momentum Closures in Ocean Models

Danilov, Sergey; Juricke, Stephan; Kutsenko, Anton; Oliver, Marcel

Pages: 145 –192

[State-of-the-art global ocean circulation models used in climate studies are only passing the edge of becoming “eddy-permitting” or barely eddy-resolving. Such models commonly suffer from overdissipation of mesoscale eddies by routinely used subgrid dissipation (viscosity) operators and a...
LitStream

Chapter 6Diagnosing and Parameterizing the Effects of Oceanic Eddies

Griesel, Alexa; Dräger-Dietel, Julia; Jochumsen, Kerstin

Pages: 193 –224

[Oceanic eddies, fluctuations on scales on the order of one km to hundreds of km, derive their energy primarily from baroclinic instability processes. Currently, climate models do not incorporate the space and time variability of the effects of eddies and sub-mesoscale processes in an...
LitStream

Chapter 7Entropy Production in Turbulence Parameterizations

Gassmann, Almut; Blender, Richard

Pages: 225 –244

[The atmosphere is a forced-dissipative system. It has to export more entropy than it imports in a steady state. Therefore, the entropy inflow and outflow have to be distinguished from the internal entropy production, which has to be positive in the mean on long timescales. This principle does...
LitStream

Chapter 8Reducing Spurious Diapycnal Mixing in Ocean Models

Klingbeil, Knut; Burchard, Hans; Danilov, Sergey; Goetz, Claus; Iske, Armin

Pages: 245 –286

[Transport algorithms of numerical ocean circulation models are frequently exhibiting truncation errors leading to spurious diapycnal mixing of water masses. This chapter discusses methods that might be useful in diagnosing spurious diapycnal mixing and describes some approaches that might be...
LitStream

Chapter 9Diffuse Interface Approaches in Atmosphere and Ocean—Modeling and Numerical Implementation

Garcke, Harald; Hinze, Michael; Kahle, Christian

Pages: 287 –307

[We propose to model physical effects at the sharp density interface between atmosphere and ocean with the help of diffuse interface approaches for multiphase flows with variable densities. We use the thermodynamical consistent variable density model proposed in Abels et al. (Mathematical Models...

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