Tritium Minority Heating With Mode Conversion Of Fast Waves

2008 ◽  
Author(s):  
C. Castaldo ◽  
A. Cardinali ◽  
Olivier Sauter ◽  
Xavier Garbet ◽  
Elio Sindoni
Keyword(s):  
Mode Conversion ◽  
Fast Waves

Observation of ion‐cyclotron heating due to mode conversion of fast waves in a simple mirror

1992 ◽  
Vol 4 (6) ◽  
pp. 1486-1491 ◽  
Author(s):  
Y. Yasaka ◽  
H. Takeno ◽  
A. Fukuyama ◽  
T. Toyoda ◽  
M. Miyakita ◽  
...  
Keyword(s):  
Mode Conversion ◽  
Ion Cyclotron ◽  
Fast Waves

Tritium minority heating with mode conversion of fast waves

2010 ◽  
Vol 17 (7) ◽  
pp. 072513 ◽  
Author(s):  
Carmine Castaldo ◽  
Alessandro Cardinali
Keyword(s):  
Mode Conversion ◽  
Fast Waves

AN EXPERIMENT WHICH MEASURES RESONANT MODE CONVERSION IN He II

1978 ◽  
Vol 39 (C6) ◽  
pp. C6-228-C6-229
Author(s):  
S. Garrett ◽  
S. Adams ◽  
S. Putterman ◽  
I. Rudnick
Keyword(s):  
Mode Conversion ◽  
Resonant Mode

Getting Rid of Fast Waves: Slow Dynamics

2018 ◽  
Author(s):  
Vladimir Zeitlin
Keyword(s):  
Rossby Waves ◽  
Baroclinic Instability ◽  
Nonlinear Effects ◽  
Kelvin Wave ◽  
Beta Plane ◽  
Equatorial Wave ◽  
Flow Over Topography ◽  
Wave Guides ◽  
Rotating Shallow Water ◽  
Fast Waves

After analysis of general properties of horizontal motion in primitive equations and introduction of principal parameters, the key notion of geostrophic equilibrium is introduced. Quasi-geostrophic reductions of one- and two-layer rotating shallow-water models are obtained by a direct filtering of fast inertia–gravity waves through a choice of the time scale of motions of interest, and by asymptotic expansions in Rossby number. Properties of quasi-geostrophic models are established. It is shown that in the beta-plane approximations the models describe Rossby waves. The first idea of the classical baroclinic instability is given, and its relation to Rossby waves is explained. Modifications of quasi-geostrophic dynamics in the presence of coastal, topographic, and equatorial wave-guides are analysed. Emission of mountain Rossby waves by a flow over topography is demonstrated. The phenomena of Kelvin wave breaking, and of soliton formation by long equatorial and topographic Rossby waves due to nonlinear effects are explained.

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