The H3+ ion:: a remote diagnostic of the jovian magnetosphere

被引:60
作者
Connerney, JEP
Satoh, T
机构
[1] NASA, Extraterr Phys Lab, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[2] Sci Univ Tokyo, Frontier Res Ctr Computat Sci, Noda, Chiba 2788510, Japan
来源
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES | 2000年 / 358卷 / 1774期
关键词
infrared; H-3(+); magnetosphere; Jupiter; auroral; Io;
D O I
10.1098/rsta.2000.0661
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Observations of the jovian system in the near-infrared (3.4 mu m) reveal a wealth of information about Jupiter's magnetic field, magnetosphere, and magnetospheric dynamics. This wavelength contains a few emission lines of the H-3(+) ion and it is centred on a deep methane absorption hand. As a result, one can image Jupiter's ionosphere at this wavelength with extraordinary signal-to-noise ratio, against a planet otherwise darkened by absorption due to methane in its atmosphere. High spatial resolution images of the planet's surface provide a synoptic view of the entire magnetosphere, fr-om the electrodynamics of Io and the torus, to the excitation of auroral displays at high magnetic latitude. Observations of the Io Flux Tube footprint have provided a new magnetic coordinate system for the jovian polar regions and new insight into the electrodynamic interaction between Jupiter and Io. Short-term temporal variations (days) of auroral intensity are observed in the IR and are well correlated with variations in the solar-wind ram pressure arriving at Jupiter. These H-3(+) emissions are thermally excited and are a good proxy for time-averaged energy deposition. It is now possible to produce detailed maps of energy deposition from the Io footprint (L = 6) to the pole, in which both system III and local time variations are evident.
引用
收藏
页码:2471 / 2483
页数:13
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