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Analysis of pioneer venus orbiter ultraviolet spectrometer lyman. alpha. data from near the subsolar region

Journal Article · · Journal of Geophysical Research; (United States)
;  [1];  [2]
  1. E.O. Hulburt Center for Space Research, Washington, DC (United States)
  2. Univ. of Colorado, Boulder (United States)
Atomic hydrogen is an important tracer not only of global atmospheric behavior, but also of the evolutionary processes which modify a planetary atmosphere. One of the most important questions in the field of the evolution of planetary atmospheres is whether or not Venus at one time had an ocean. The answer is directly related to the present, and past, escape flux of atomic hydrogen. Techniques for determining the abundance of atomic hydrogen are somewhat limited, and those for determining the flux of escaping hydrogen even more so. Pioneer Venus Orbiter ultraviolet spectrometer data from 20 orbits which span 3 years have been analyzed to determine the atomic hydrogen number density and vertical flux at the exobase as a function of solar zenith angle, F{sub 10.7} index, and spacecraft latitude. From 1979 through 1981 the exobase number density n{sub c} and flux {phi}{sub c} are remarkably constant at n{sub c} = 6.0 {+-} 1.5 {times} 10{sup 4} cm{sup {minus}3} and {phi}{sub c} = 7.5 {+-} 1.5 {times} 10{sup 7} cm{sup {minus}2} s{sup {minus}1} in the subsolar region. The integrated vertical column density above 110 km is 3.6 {+-} 1 {times} 10{sup 13} cm{sup {minus}2}. An empirical relationship is determined between the line center solar flux at H Lyman {alpha}, {pi}F{sub o}, and the F{sub 10.7} index. At 1 AU, {pi}F{sub o} = (2.0 + 1.1 {times} 10{sup {minus}2}F{sub 10.7}) {times} 10{sup 11} photons cm{sup {minus}2} s{sup {minus}1} {angstrom}{sup {minus}1}.
OSTI ID:
6050981
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 93:A3; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English