Title of article :
X-rays from solar system objects
Author/Authors :
Bhardwaj، نويسنده , , Anil and Elsner، نويسنده , , Ronald F. and Randall Gladstone، نويسنده , , G. and Cravens، نويسنده , , Thomas E. and Lisse، نويسنده , , Carey M. and Dennerl، نويسنده , , Konrad and Branduardi-Raymont، نويسنده , , Graziella and Wargelin، نويسنده , , Bradford J. and Hunter Waite Jr.، نويسنده , , J. and Robertson، نويسنده , , Ina and طstgaard، نويسنده , , Nikolai and، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2007
Abstract :
During the last few years our knowledge about the X-ray emission from bodies within the solar system has significantly improved. Several new solar system objects are now known to shine in X-rays at energies below 2 keV. Apart from the Sun, the known X-ray emitters now include planets (Venus, Earth, Mars, Jupiter, and Saturn), planetary satellites (Moon, Io, Europa, and Ganymede), all active comets, the Io plasma torus (IPT), the rings of Saturn, the coronae (exospheres) of Earth and Mars, and the heliosphere. The advent of higher-resolution X-ray spectroscopy with the Chandra and XMM-Newton X-ray observatories has been of great benefit in advancing the field of planetary X-ray astronomy. Progress in modeling X-ray emission, laboratory studies of X-ray production, and theoretical calculations of cross-sections, have all contributed to our understanding of processes that produce X-rays from the solar system bodies.
iter and Earth, both auroral and non-auroral disk X-ray emissions have been observed. X-rays have been detected from Saturnʹs disk, but no convincing evidence of an X-ray aurora has been observed. The first soft (0.1–2 keV) X-ray observation of Earthʹs aurora by Chandra shows that it is highly variable. The non-auroral X-ray emissions from Jupiter, Saturn, and Earth, those from the disk of Mars, Venus, and Moon, and from the rings of Saturn, are mainly produced by scattering of solar X-rays. The spectral characteristics of X-ray emission from comets, the heliosphere, the geocorona, and the Martian halo are quite similar, but they appear to be quite different from those of Jovian auroral X-rays. X-rays from the Galilean satellites and the IPT are mostly driven by impact of Jovian magnetospheric particles.
aper reviews studies of the soft X-ray emission from the solar system bodies, excluding the Sun. Processes of production of solar system X-rays are discussed and an overview is provided of the main source mechanisms of X-ray production at each object. A brief account on recent development in the area of laboratory studies of X-ray production is also provided.
Keywords :
X-ray emission , solar wind , heliosphere , atmosphere , planets , Minor bodies , Planetary satellites , comets
Journal title :
PLANETARY AND SPACE SCIENCE
Journal title :
PLANETARY AND SPACE SCIENCE