Absorption and emission of plasma waves in mode conversion layers at general harmonics of the ion cyclotron frequency

1990 ◽  
Vol 2 (11) ◽  
pp. 2693-2703 ◽  
Author(s):  
Suwon Cho ◽  
D. G. Swanson
2008 ◽  
Vol 101 (23) ◽  
Author(s):  
Y. Lin ◽  
J. E. Rice ◽  
S. J. Wukitch ◽  
M. J. Greenwald ◽  
A. E. Hubbard ◽  
...  

2012 ◽  
Vol 54 (3) ◽  
pp. 035005 ◽  
Author(s):  
W Y Zhang ◽  
Y D Li ◽  
X J Zhang ◽  
T Lan ◽  
X Gao ◽  
...  

2009 ◽  
Vol 16 (2) ◽  
pp. 319-329 ◽  
Author(s):  
C. Briand

Abstract. Since the very beginning of the space venture, discrepancies between hydrodynamic models and observations have raised the attention to the kinetic effects taking place in the interplanetary medium. After discussing some of these constraints, a review on the state of the art knowledge on the waves in the range fci<f<fpe (fci – about 10−1 Hz – is the ion cyclotron frequency, and fpe – a few 10 kHz – the electron plasma frequency) observed in the free solar wind, i.e., not magnetically connected to the Earth's bow shock, is addressed.


1999 ◽  
Vol 17 (6) ◽  
pp. 712-722 ◽  
Author(s):  
C. Vocks ◽  
U. Motschmann ◽  
K.-H. Glassmeier

Abstract. A filter method is presented which allows a qualitative and quantitative identification of wave modes observed with plasma experiments on satellites. Hitherto existing mode filters are based on the MHD theory and thus they are restricted to low frequencies well below the ion cyclotron frequency. The present method is generalized to cover wave modes up to the characteristic ion frequencies. The spectral density matrix determined by the observations is decomposed using the eigenvectors of the linearized Hall-MHD equations. As the wave modes are dispersive in this formalism, a precise determination of the k->-vectors requires the use of multi-point measurements. Therefore the method is particularly relevant to multi-satellite missions. The method is tested using simulated plasma data. The Hall-MHD filter is able to identify the modes excited in the model plasma and to assign the correct energetic contributions. By comparison with the former method it is shown that the simple MHD filter leads to large errors if the frequency is not well below the ion cyclotron frequency. Further the range of validity of the linear theory is examined rising the simulated wave amplitudes.Key words. Magnetospheric physics (MHD waves and instabilities; plasma waves and instabilities)


2012 ◽  
Vol 30 (1) ◽  
pp. 97-107 ◽  
Author(s):  
S. Y. Huang ◽  
M. Zhou ◽  
X. H. Deng ◽  
Z. G. Yuan ◽  
Y. Pang ◽  
...  

Abstract. Multiple dipolarization fronts (DFs) were observed by Cluster spacecraft in the magnetotail during a substorm. These DFs were kinetic structures, embedded in the bursty plasma flow, and moved earthward (mainly) and dawnward. Intense electric field, parallel and perpendicular currents were detected in the DF layer. These front layers were energy dissipation region (load region) where the energy of electromagnetic fields were transferred to the plasma thermal and kinetic energy. This dissipation was dominated by electrons. There were enhancements of plasma waves around the DF region: wavelet results show that wave activities around the ion cyclotron frequency in the front layer were generated by Alfvén ion cyclotron instability; whistler waves were also detected before, during and after the DFs, which are triggered by electron temperature anisotropy and coincident with enhancement of energetic electron fluxes. The observation of these waves could be important for the understanding of evolution of DF and electron energization during the substorm. We discuss the generation mechanism of the DFs and suggest that these DFs were generated in the process of transient reconnection, and then traveled toward the Earth.


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