The H-3(+) ion: a remote diagnostic of the jovian magnetosphere

Citation
Jep. Connerney et T. Satoh, The H-3(+) ion: a remote diagnostic of the jovian magnetosphere, PHI T ROY A, 358(1774), 2000, pp. 2471-2483
Citations number
49
Categorie Soggetti
Multidisciplinary
Journal title
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES
ISSN journal
1364503X → ACNP
Volume
358
Issue
1774
Year of publication
2000
Pages
2471 - 2483
Database
ISI
SICI code
1364-503X(20000915)358:1774<2471:THIARD>2.0.ZU;2-L
Abstract
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 ma gnetospheric 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 resul t, one can image Jupiter's ionosphere at this wavelength with extraordinary signal-to-noise ratio, against a planet otherwise darkened by absorption d ue to methane in its atmosphere. High spatial resolution images of the plan et'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. Sh ort-term temporal variations (days) of auroral intensity are observed in th e 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 pro duce detailed maps of energy deposition from the Io footprint (L = 6) to th e pole, in which both system III and local time variations are evident.