HIGH-RESOLUTION ULTRAVIOLET SPECTROSCOPY OF JUPITER AURORA WITH THE HUBBLE-SPACE-TELESCOPE

被引:27
|
作者
KIM, YH
CALDWELL, JJ
FOX, JL
机构
[1] UNIV MARYLAND,DEPT ASTRON,COLLEGE PK,MD 20742
[2] YORK UNIV,INST SPACE & TERR SCI,N YORK,ON M3J 3K1,CANADA
[3] SUNY STONY BROOK,INST ATMOSPHER SCI,STONY BROOK,NY 11794
来源
ASTROPHYSICAL JOURNAL | 1995年 / 447卷 / 02期
关键词
LINE; FORMATION; MOLECULAR PROCESSES; PLANETS AND SATELLITES; INDIVIDUAL; (JUPITER); ULTRAVIOLET; SOLAR SYSTEM;
D O I
10.1086/175928
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
In 1993 June and July, we obtained 18 spectra of Jupiter's aurora in the wavelength range 1586-1620 Angstrom using the Goddard High Resolution Spectrograph on board the Hubble Space Telescope (HST). The field of view for each observation was 2 '' x 2 ''. There were 14 spectra of the northern and four spectra of the southern auroral ovals. The spectra are dominated by vibrational-rotational lines of the H-2 Lyman band system, from which we have determined H-2 rotational temperatures which correspond to the altitude region where most of the auroral emission originates. Intense emission was observed in two spectra at longitude 155 degrees-165 degrees, latitude 50 degrees-65 degrees, at a time when the central meridian longitude was near 190 degrees. This location coincides with a bright spot in HST Faint Object Camera images of Jupiter's northern aurora. We estimate total emission rates in the Lyman band system of similar to 250 kR for the bright regions and similar to 25-130 kR for the fainter regions. The best-fit temperatures for the bright region and fainter regions are in the ranges 200-500 K and 200-800 K, respectively. The relatively low temperatures for the bright regions may indicate that the precipitating primary particles responsible for UV emission there penetrate more deeply than do particles in the fainter regions, to altitudes where the temperatures are lower because of efficient cooling by hydrocarbons.
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页码:906 / 914
页数:9
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