1971
DOI: 10.1029/ja076i028p06666
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Mariner 6 and 7 Ultraviolet Spectrometer Experiment: Analysis of hydrogen Lyman-alpha data

Abstract: Mariner 6 and 7 ultraviolet spectrometers that flew by Mars in 1969 observed the Lyman‐α dayglow of atomic hydrogen. Data in the altitude range 200 to 24,000 km are analyzed to determine the structure of the Martian exosphere. The classical evaporative theory is applied to calculate a hydrogen density distribution. A spherical model of the dayglow Lyman‐α emission, using radiative transfer theory, is used to produce theoretical intensities for comparison with the data in order to determine temperature and dens… Show more

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Cited by 215 publications
(144 citation statements)
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“…The error bars of the Mariner values are notably smaller because the Mariner measurements were obtained with a UV spectrometer that was designed for this task. Since our interpretation of the Mariner measurements is consistent with the one published 35 years ago by Anderson and Hord (1971) we conclude that the values derived from UV airglow measurements do not critically depend on the specific exosphere model. (20) to (25)), whereas for the three lower rows we have assumed the co-existence of a cool and a hot hydrogen component.…”
Section: One Single Hydrogen Componentsupporting
confidence: 76%
“…The error bars of the Mariner values are notably smaller because the Mariner measurements were obtained with a UV spectrometer that was designed for this task. Since our interpretation of the Mariner measurements is consistent with the one published 35 years ago by Anderson and Hord (1971) we conclude that the values derived from UV airglow measurements do not critically depend on the specific exosphere model. (20) to (25)), whereas for the three lower rows we have assumed the co-existence of a cool and a hot hydrogen component.…”
Section: One Single Hydrogen Componentsupporting
confidence: 76%
“…Mariner 10 measurements of the He corona gave a T o of about 375 + 105 K . Anderson (1976) reanalyzed the Mariner 5 Lc~ data and reported for the inner component a dayside temperature of 275 K and a nightside temperature of 150 K. These low values were later confirmed by the Pioneer Venus in situ measurements. A value of T o of 275 + 15 K was derived from the He densities measured by the Bus Neutral Mass Spectrometer at 08" 30 local time, 37.9 ~ S latitude (von Zahn et al, 1980).…”
Section: Exospheric Temperaturementioning
confidence: 96%
“…For hydrogen, the density profile used is a combination of results from Anderson & Hord (1971) and Krasnopolsky (2002): …”
Section: Solar Parametersmentioning
confidence: 99%