Atmospheric hydrogen physical chemistry: The Jupiter and Uranus dayglows

Details Atmospheric hydrogen physical chemistry: The Jupiter and Uranus dayglows Atmospheric hydrogen physical chemistry: The Jupiter and Uranus dayglows

May 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003dps....35.5012s&link_type=abstract

American Astronomical Society, DPS meeting #35, #50.12; Bulletin of the American Astronomical Society, Vol. 35, p.1020

Astronomy and Astrophysics

Astronomy

1

Scientific paper

A hydrogen physical chemistry model operating at the rotational structure level has been developed for application to the outer planet atmospheres. The model has been applied to a preliminary analysis of the Cassini UVIS observations of the Jupiter dayglow, and to comparison with the H2 quadrupole emissions obtained by Trafton in observations of Uranus. The Jupiter EUV/FUV H2 band emissions show dominance by very cold electron excitation mixed with solar photon flux fluorescence. The major source of emission is exospheric. The spectra show strong Rydberg series lines excited primarily also by cold electrons in the exosphere. The model predicts dominance of H3+ throughout the ionosphere with the exception of the extreme upper exosphere. The H2 predicted ground state vibrational and rotational population is damped by the ambient ionosphere electrons, but the activated gas shows populations as much as 10 to 15 orders of magnitude above LTE. H2 vibrational populations are forced by a positive feedback system in one branch of the recombination of H3+, by hot atomic hydrogen collisions with H2, and 3-body recombination of atomic hydrogen. Uranus, with lower ionosphere densities, is predicted to be more efficient in building H2 substantial ground state vibration populations. The present model, however, falls far short of predicting the observed H2 quadrupole emission power at Uranus, we believe primarily because the H + H2 vibrational excitation reaction is not fully incorporated into the model architecture. The determination of the extent of the role of direct solar input in the development of the dayglow will be determined only by a top-down ionospheric model calculation in order to define photoionization rates in vibrationally excited H2. On the basis of these calculations, heating of the upper thermospheres is primarily determined by electron impact dissociation of vibrationally excited H2. Funding for this work is supported by Cassini Program support of the UVIS experiment, and NASA Grant NAG5-8939 to the University of Southern California.

Affiliated with

Also associated with

No associations

Rating

Atmospheric hydrogen physical chemistry: The Jupiter and Uranus dayglows does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Atmospheric hydrogen physical chemistry: The Jupiter and Uranus dayglows, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Atmospheric hydrogen physical chemistry: The Jupiter and Uranus dayglows will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1523551