Plasma environment of Jupiter family comets

被引:38
作者
Coates, A. J. [1 ,2 ]
Jones, G. H. [1 ,2 ]
机构
[1] Univ Coll London, Mullard Space Sci Lab, Dorking RH5 6NT, Surrey, England
[2] UCL Birkbeck, Ctr Planetary Sci, London WC1E 6BT, England
关键词
Comets; Solar wind; Ion pickup; SOLAR-WIND INTERACTION; WATER-GROUP IONS; VELOCITY SPACE DIFFUSION; P-GRIGG-SKJELLERUP; PILE-UP REGION; GIOTTO MAGNETOMETER EXPERIMENT; MAGNETIC-FIELD OBSERVATIONS; CORONAL MASS EJECTION; X-RAY-EMISSION; PICKUP IONS;
D O I
10.1016/j.pss.2009.04.009
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
As any comet nears the Sun, gas sublimes from the nucleus taking dust with it. Jupiter family comets are no exception. The neutral gas becomes ionized, and the interaction of a comet with the solar wind starts with ion pickup. This key process is also important in other solar system contexts wherever neutral particles become ionized and injected into a flowing plasma such as at Mars, Venus, Io, Titan and interstellar neutrals in the solar wind. At comets, ion pickup removes momentum and energy from the solar wind and puts it into cometary particles, which are then thermalised via plasma waves. Here we review what comets have shown us about how this process operates, and briefly look at how this can be applied in other contexts. We review the processes of pitch angle and energy scattering of the pickup ions, and the boundaries and regions in the comet-solar wind interaction. We use in-situ measurements from the four comets visited to date by spacecraft carrying plasma instrumentation: 21P/Giacobini-Zinner, 1P/Halley, 26P/Grigg-Skjellerup and 19P/Borrelly, to illustrate the process in action. While, of these, comet Halley is not a Jupiter class comet, it has told us the most about cometary plasma environments. The other comets, which are from the Jupiter family, give an interesting comparison as they have lower gas production rates and less-developed interactions. We examine the prospects for Rosetta at comet Churyumov-Gerasimenko, another Jupiter family comet where a wide range of gas production rates will be studied. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1175 / 1191
页数:17
相关论文
共 141 条
[1]   Magnetic field and plasma observations at Mars:: Initial results of the Mars global surveyor mission [J].
Acuña, MH ;
Connerney, JEP ;
Wasilewski, P ;
Lin, RP ;
Anderson, KA ;
Carlson, CW ;
McFadden, J ;
Curtis, DW ;
Mitchell, D ;
Reme, H ;
Mazelle, C ;
Sauvaud, JA ;
d'Uston, C ;
Cros, A ;
Medale, JL ;
Bauer, SJ ;
Cloutier, P ;
Mayhew, M ;
Winterhalter, D ;
Ness, NF .
SCIENCE, 1998, 279 (5357) :1676-1680
[2]   ON THE THEORY OF COMET TAILS [J].
ALFVEN, H .
TELLUS, 1957, 9 (01) :92-96
[3]  
ALTWEGG K, 1993, ASTRON ASTROPHYS, V279, P260
[4]  
ALTWEGG K, 2008, SPACE SCI REV, V138
[5]   ENERGIZATION OF POSITIVE-IONS IN THE COMETARY FORESHOCK REGION [J].
AMATA, E ;
FORMISANO, V .
PLANETARY AND SPACE SCIENCE, 1985, 33 (11) :1243-1250
[6]  
AMATA E, 1986, ESA SP2501 EUR SPAC, P213
[7]   ION COMPOSITION AND DYNAMICS AT COMET HALLEY [J].
BALSIGER, H ;
ALTWEGG, K ;
BUHLER, F ;
GEISS, J ;
GHIELMETTI, AG ;
GOLDSTEIN, BE ;
GOLDSTEIN, R ;
HUNTRESS, WT ;
IP, WH ;
LAZARUS, AJ ;
MEIER, A ;
NEUGEBAUER, M ;
RETTENMUND, U ;
ROSENBAUER, H ;
SCHWENN, R ;
SHARP, RD ;
SHELLEY, EG ;
UNGSTRUP, E ;
YOUNG, DT .
NATURE, 1986, 321 (6067) :330-334
[8]  
BALSIGER H, 1990, COMET HALLEY INVESTI, V1
[9]  
BIERMANN L, 1951, Z ASTROPHYS, V29, P274
[10]  
Biermann L., 1967, Sol. Phys, V1, P254, DOI [10.1007/BF00150860, DOI 10.1007/BF00150860]