PLASMA ENERGIZATION BY THE PONDEROMOTIVE FORCE OF MAGNETOSPHERIC STANDING ALFVEN WAVES

被引:28
作者
ALLAN, W [1 ]
机构
[1] NATL INST WATER & ATMOSPHER RES LTD, POB 31-311, LOWER HUTT, NEW ZEALAND
关键词
D O I
10.1029/93JA00728
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The second-order force generated by standing Alfven waves in a dipolar magnetospheric geometry is rederived in a more straightforward and accurate way than previously done. The spatial structure of the resulting ponderomotive acceleration consists of regions in which plasma can be trapped between ''diverging'' nodes of the acceleration field (where the acceleration vector points away form the node). The ''specific parallel energy'' (parallel energy per proton mass) of accelerated plasma particles is derived. The quantity maximized at ''converging'' nodes of the acceleration field (where the acceleration vector points toward the node). For the fundamental standing mode the converging node is at the equatorial plane, and the maximum specific energy there increases rapidly with L(where L is the McIlwain parameter), becoming significant above L = 5 for typical wave amplitudes. At L approximately 10, H+ ions should reach energies of approximately 100 eV and O+ ions energies of approximately 2 keV. Gravity has little effect on the energization, other than to define the magnetic latitude from which acceleration begins. AT reasonably high L, almost all the energization occurs at magnetic latitudes above +/- 45-degrees. For the second harmonic the converging nodes are situated away from the equatorial plane, and accelerated particles starting from rest do not reach that plane. The third harmonic has a converging node at the equatorial plane, and specific energies there are the same as for the fundamental mode. However, the accelerated particles originate from above the diverging nodes at latitudes of about +/- 18-degrees, passing through a larger acceleration field than for the fundamental mode in that region. Particles having initial energies of a few electron volts near the ionosphere may be able to traverse the diverging nodes of the third harmonic and reach the equatorial plane.
引用
收藏
页码:11383 / 11390
页数:8
相关论文
共 21 条
[1]   DOES THE PONDEROMOTIVE FORCE MOVE MASS IN THE MAGNETOSPHERE [J].
ALLAN, W ;
MANUEL, JR ;
POULTER, EM .
GEOPHYSICAL RESEARCH LETTERS, 1990, 17 (07) :917-920
[3]   PONDEROMOTIVE MASS-TRANSPORT IN THE MAGNETOSPHERE [J].
ALLAN, W .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1992, 97 (A6) :8483-8493
[4]   MAGNETOSPHERIC CAVITY MODES - SOME NONLINEAR EFFECTS [J].
ALLAN, W ;
MANUEL, JR ;
POULTER, EM .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1991, 96 (A7) :11461-11473
[5]   SPATIAL AND TEMPORAL STRUCTURE OF A HIGH-LATITUDE TRANSIENT ULF PULSATION [J].
ALLAN, W ;
POULTER, EM ;
GLASSMEIER, KH ;
JUNGINGER, H .
PLANETARY AND SPACE SCIENCE, 1985, 33 (02) :159-173
[6]   WHAT PARTS OF BROAD-BAND SPECTRA ARE RESPONSIBLE FOR ION CONIC PRODUCTION [J].
BALL, L ;
ANDRE, M .
GEOPHYSICAL RESEARCH LETTERS, 1991, 18 (09) :1683-1686
[7]   HIGH-RESOLUTION SOUNDING ROCKET OBSERVATIONS OF LARGE-AMPLITUDE ALFVEN WAVES [J].
BOEHM, MH ;
CARLSON, CW ;
MCFADDEN, JP ;
CLEMMONS, JH ;
MOZER, FS .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1990, 95 (A8) :12157-12171
[8]   ARC-LENGTHS ALONG THE LINES OF FORCE OF A MAGNETIC DIPOLE [J].
CHAPMAN, S ;
SUGIURA, M .
JOURNAL OF GEOPHYSICAL RESEARCH, 1956, 61 (03) :485-488
[9]   INTERACTION BETWEEN HYDROMAGNETIC WAVES AND A TIME-DEPENDENT, INHOMOGENEOUS MEDIUM [J].
DEWAR, RL .
PHYSICS OF FLUIDS, 1970, 13 (11) :2710-&
[10]   NONLINEAR GENERATION OF ION HOLES IN AURORAL PLASMAS [J].
LAKHINA, GS ;
SHUKLA, PK ;
VERHEEST, F .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1992, 97 (A6) :8355-8359