Ground based images obtained hourly by seven observatories are used to study Martian phenomena. Maps of global dust storms show the degree of activity of the storm depends both on the region and on the time of day. Statistical analysis of regional contrast variations on the images supports the opinion that the contrasts in the brightness of the light and dark areas depends on the Martian season. Residual differences may be due to a phase angle dependence. Diagrams confirm the earlier finding that there is a systematic trend of regional contrast with the time of the Martian day and that the afternoon is not symmetric with the morning. The dissipation of Martian polar caps is also discussed
Calculations of the daily solar radiation incident at the tops of the atmospheres of Mars and the ou...
Daily global imaging by the Mars Color Imager (MARCI) continues the record of the Mars Orbiter Camer...
The meteorological excitation of Mars' rotation refers to the change of Mars' orientation parameters...
Extensive Earth-based photography of Mars, Jupiter, and Venus is presented which monitors the atmosp...
The purpose is to determine the degree, spatial distribution and timing of the deposition and remova...
We show that the dust devil parameterisation in use in most Mars Global Circulation Models (MGCMs) r...
It is reported that on the global scale, no major dust storm activity was seen during telescopic obs...
Dust devils are vortices of air made visible by entrained dust particles. Dust devils have been obse...
Dust devils are vortices of air made visible by entrained dust particles. Dust devils have been obse...
Transient phenomena on Mars have long been recognized in Mariner and Viking images as well as in dec...
Following earlier work to map the dust opacity of the Mars atmosphere, a number of separate studies ...
The possible indicators of impending Martian dust storms are discussed. Topics covered include the f...
International audienceThis paper presents a monitoring of the atmospheric dust in the south polar re...
A possible initiation mechanism for global dust storms was raised by describing a new analysis of wi...
Like Earth, Mars has polar vortices: regions of cold air above the winter pole, circumscribed by pow...
Calculations of the daily solar radiation incident at the tops of the atmospheres of Mars and the ou...
Daily global imaging by the Mars Color Imager (MARCI) continues the record of the Mars Orbiter Camer...
The meteorological excitation of Mars' rotation refers to the change of Mars' orientation parameters...
Extensive Earth-based photography of Mars, Jupiter, and Venus is presented which monitors the atmosp...
The purpose is to determine the degree, spatial distribution and timing of the deposition and remova...
We show that the dust devil parameterisation in use in most Mars Global Circulation Models (MGCMs) r...
It is reported that on the global scale, no major dust storm activity was seen during telescopic obs...
Dust devils are vortices of air made visible by entrained dust particles. Dust devils have been obse...
Dust devils are vortices of air made visible by entrained dust particles. Dust devils have been obse...
Transient phenomena on Mars have long been recognized in Mariner and Viking images as well as in dec...
Following earlier work to map the dust opacity of the Mars atmosphere, a number of separate studies ...
The possible indicators of impending Martian dust storms are discussed. Topics covered include the f...
International audienceThis paper presents a monitoring of the atmospheric dust in the south polar re...
A possible initiation mechanism for global dust storms was raised by describing a new analysis of wi...
Like Earth, Mars has polar vortices: regions of cold air above the winter pole, circumscribed by pow...
Calculations of the daily solar radiation incident at the tops of the atmospheres of Mars and the ou...
Daily global imaging by the Mars Color Imager (MARCI) continues the record of the Mars Orbiter Camer...
The meteorological excitation of Mars' rotation refers to the change of Mars' orientation parameters...