Results of investigation of probable atmospheric effects appearing in Mariner '69 TV pictures that have undergone noise removal and preliminary decalibration are described. Two distinct types of haze are distinguished: north polar haze, seen prominently against the face of the planet in blue photographs, and thin haze, usually identified by its appearance on the limb and not strongly colored. Thin haze is surprisingly widespread, particularly in the southern hemisphere. Discrete bright features, which may be evidence for condensation on the ground or in the atmosphere, are described. These occur where bright features have often been seen from earth, in a region where very large multiple-ringed structures seem to dominate the surface morphol...
A total of 201 complete television frames of Mars were returned by Mariners 6 and 7 in late July and...
The interface between certain geological and atmospheric phenomena on Mars was studied by examining ...
Whenever Viking Orbiter images included the limb of Mars, they recorded one or more layers of clouds...
Model explaining brightness and haze in Mars photographs obtained by Mariner 4 spacecraf
Photometric investigation of haze in Mars atmosphere revealed by Mariner 4 television dat
Progress on a project to elucidate the geological and topographic setting of the Martian polar volat...
Data from six Mariner Mars experiments are presented. Television reconnaissance of Mars and its sate...
Transient phenomena on Mars have long been recognized in Mariner and Viking images as well as in dec...
The effects of the Martian atmosphere on an optical communication link are analyzed using Mariner 9,...
The Mariner 6 and 7 pictures have provided significant clues to the nature of the light and dark mar...
The amount of dust suspended in the Martian atmosphere is highly variable with location and with tim...
The Mariner 9 encounter with Mars is extensively documented with photographs taken by the satellite'...
Viking lander camera images of the Sun were used to compute atmospheric optical depth at two sites o...
At orbit insertion on 14 November 1971 the Martian surface was largely obscured by a dust haze with ...
The Martian atmosphere often shows horizontal layers of haze up to altitudes of about 80 km. The Hig...
A total of 201 complete television frames of Mars were returned by Mariners 6 and 7 in late July and...
The interface between certain geological and atmospheric phenomena on Mars was studied by examining ...
Whenever Viking Orbiter images included the limb of Mars, they recorded one or more layers of clouds...
Model explaining brightness and haze in Mars photographs obtained by Mariner 4 spacecraf
Photometric investigation of haze in Mars atmosphere revealed by Mariner 4 television dat
Progress on a project to elucidate the geological and topographic setting of the Martian polar volat...
Data from six Mariner Mars experiments are presented. Television reconnaissance of Mars and its sate...
Transient phenomena on Mars have long been recognized in Mariner and Viking images as well as in dec...
The effects of the Martian atmosphere on an optical communication link are analyzed using Mariner 9,...
The Mariner 6 and 7 pictures have provided significant clues to the nature of the light and dark mar...
The amount of dust suspended in the Martian atmosphere is highly variable with location and with tim...
The Mariner 9 encounter with Mars is extensively documented with photographs taken by the satellite'...
Viking lander camera images of the Sun were used to compute atmospheric optical depth at two sites o...
At orbit insertion on 14 November 1971 the Martian surface was largely obscured by a dust haze with ...
The Martian atmosphere often shows horizontal layers of haze up to altitudes of about 80 km. The Hig...
A total of 201 complete television frames of Mars were returned by Mariners 6 and 7 in late July and...
The interface between certain geological and atmospheric phenomena on Mars was studied by examining ...
Whenever Viking Orbiter images included the limb of Mars, they recorded one or more layers of clouds...