Show simple item record

contributor authorBarth, Charles A.
date accessioned2017-06-09T14:14:29Z
date available2017-06-09T14:14:29Z
date copyright1968/07/01
date issued1968
identifier issn0022-4928
identifier otherams-15458.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151132
description abstractThe Mariner 5 Lyman alpha measurements can be fitted with the barometric-exospheric equation only if a two-component model atmosphere is used. Of the three possible hypotheses to explain such an atmosphere, the model containing a mixture of atomic hydrogen and molecular hydrogen is preferred over the atomic hydrogen-deuterium model or the atomic hydrogen two-temperature model. The source of molecular hydrogen in the upper atmosphere may be chemical reactions either in the hot, dense lower atmosphere or in the upper atmosphere. The photodissociation of molecular hydrogen produces atoms with excess kinetic energy which either escape from the planetary gravitational field or react with the molecules in the lower atmosphere. The presence of molecular hydrogen affects calculations of the temperature of the Venus upper atmosphere as well as its ionic and chemical structure.
publisherAmerican Meteorological Society
titleInterpretation of the Mariner 5 Lyman Alpha Measurements
typeJournal Paper
journal volume25
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1968)025<0564:IOTMLA>2.0.CO;2
journal fristpage564
journal lastpage567
treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 004
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record