Skip to search formSkip to main contentSkip to account menu
  • Publications
  • Influence
The roughness of natural terrain: A planetary and remote sensing perspective
We examine the various methods and parameters in common use for quantifying and reporting surface topographic “roughness.” It is shown that scale-dependent roughness parameters are almost always…
View via Publisher
SHARAD sounding radar on the Mars Reconnaissance Orbiter
[1] SHARAD (SHAllow RADar) is a sounding radar provided by Agenzia Spaziale Italiana (ASI) as a Facility Instrument on the Mars Reconnaissance Orbiter mission. Its 20-MHz center frequency and 10-MHz…
View via Publisher
Global distribution of near-surface hydrogen on Mars
[1] Neutron data observed using the Neutron Spectrometer aboard 2001 Mars Odyssey provide a lower limit to the global inventory of Martian water-equivalent hydrogen. Hydrogen-rich deposits ranging…
View via Publisher
Variation of the Martian Ionospheric Electron Density from Mars Express Radar Soundings
[1] The Mars Advanced Radar for Subsurface and Ionospheric Sounding aboard Mars Express has been in operation for over 2 years. Between 14 August 2005 and 31 July 2007, we obtain 34,492 ionospheric…
View via Publisher
Subsurface Radar Sounding of the South Polar Layered Deposits of Mars
TLDR
The ice-rich south polar layered deposits of Mars were probed with the Mars Advanced Radar for Subsurface and Ionospheric Sounding on the Mars Express orbiter, suggesting a composition of nearly pure water ice.
View on Publisher
Mars North Polar Deposits: Stratigraphy, Age, and Geodynamical Response
TLDR
The Shallow Radar (SHARAD) on the Mars Reconnaissance Orbiter has imaged the internal stratigraphy of the north polar layered deposits of Mars, revealing a laterally continuous deposition of layers which typically consist of four packets of finely spaced reflectors separated by homogeneous interpacket regions of nearly pure ice.
View on Publisher
Surface Ages and Resurfacing Rates of the Polar Layered Deposits on Mars
Interpretation of the polar stratigraphy of Mars in terms of global climate changes is complicated by the significant difference in surface ages between the north and south polar layered terrains…
View via Publisher
Radar Sounding Evidence for Buried Glaciers in the Southern Mid-Latitudes of Mars
TLDR
Soundings of these deposits in the eastern Hellas region by the Shallow Radar on the Mars Reconnaissance Orbiter reveal radar properties entirely consistent with massive water ice, supporting the debris-covered glacier hypothesis.
View on Publisher
Radar evidence for ice in lobate debris aprons in the mid‐northern latitudes of Mars
Subsurface radar sounding data indicate that lobate debris aprons found in Deuteronilus Mensae in the mid‐northern latitudes of Mars are composed predominantly of water ice. The position in time…
View on Wiley
Magnetically controlled structures in the ionosphere of Mars
[1] The ionospheric sounding data obtained by the MARSIS (Mars Advanced Radar for Subsurface and Ionospheric Sounding) instrument on the Mars Express spacecraft show that the dayside ionosphere has…
View via Publisher
...
...
By clicking accept or continuing to use the site, you agree to the terms outlined in our Privacy Policy, Terms of Service, and Dataset License