Results 101 to 110 of about 34,777 (278)

Near Surface Properties of Martian Regolith Derived From InSight HP³‐RAD Temperature Observations During Phobos Transits [PDF]

, 2021
Nils Mueller, S. Piqueux, M. T. Lemmon, J. N. Maki, R. D. Lorenz, M. Grott, Tilman Spohn, S. E. Smrekar, J. Knollenberg, T. L. Hudson, C. Krause, Ehouarn Millour, F. Forget, M. P. Golombek, A. Hagermann, N. Attree, M.A. Siegler, W. B. Banerdt   +17 more
openalex   +1 more source

The ISSI international study team on the martian PBL – status report and plan [PDF]

, 2008
Dynamical processes in the Martian boundary layer provide the means of communication between surface ice deposits and the free atmosphere, and the means of lifting dust from the surface.
Galperin, B., Gundersson, K., Larsen, S., Lewis, S., Petrosyan, A., Read, P., Renno, N., Richardson, M., Rogberg, P., Savijärvi, H., Seiferlin, K., Siili, T., Thomas, N., Toigo, A.   +13 more
core  

Identification of a basaltic component on the Martian surface from Thermal Emission Spectrometer data [PDF]

, 2000
P. R. Christensen, J. L. Bandfield, M. D. Smith, V. E. Hamilton, R. N. Clark   +4 more
openalex   +1 more source

Prototype Backscatter Moessbauer Spectrometer for Measurement of Martian Surface Mineralogy [PDF]

We have designed and successfully tested a prototype of a backscatter Moessbauer spectrometer (BaMS) targeted for use on the Martian surface to (1) determine oxidation states of iron, and (2) identify and determine relative abundances of iron-bearing ...
Agresti, D. G., Morris, R. V., Nguyen, T., Shelfer, T. D., Shen, M. H., Wills, E. L.   +5 more
core   +1 more source

High-frequency near-surface gas measurement: an opportunity to solve puzzles in planetary atmospheric processes in Martian Methane and beyond [PDF]

, 2021
John E. Moores, H. M. Sapers, Dorothy Z. Oehler, Claire Newman, Lyle G. Whyte   +4 more
openalex   +1 more source

Thermal tides in the Martian middle atmosphere as seen by the Mars Climate Sounder [PDF]

, 2009
The first systematic observations of the middle atmosphere of Mars (35–80km) with the Mars Climate Sounder (MCS) show dramatic patterns of diurnal thermal variation, evident in retrievals of temperature and water ice opacity.
A. D. Toigo, A. Kleinböhl, Arakawa, Banfield, Banfield, Banfield, C. B. Leovy, C. Lee, Cahoy, Chahine, Chapman, Colburn, Conrath, D. Banfield, D. J. McCleese, D. Kass, F. W. Taylor, Forbes, Forget, Gierasch, Haberle, Hamilton, Hamilton, Heavens, Hess, J. T. Schofield, Johnson, Leovy, Leovy, Leovy, Lewis, Lewis, Lieberman, M. I. Richardson, Martin, Martin, McCleese, McCleese, Murphy, N. G. Heavens, R. Zurek, Read, Richardson, Rondanelli, Salby, Salby, Schofield, Smith, Smith, Tillman, W. G. Lawson, Warren, Wilson, Wilson, Wilson, Wilson, Wilson, Zurek, Zurek, Zurek, Zurek, Zurek   +61 more
core   +1 more source

From the Martian Surface to Its Low Orbit in a Reusable Single-Stage Vehicle—Charon [PDF]

, 2021
Jérémie Gaffarel, Afrasiab Kadhum, Mohammad Fazaeli, Dimitrios Apostolidis, Menno Berger, Lukas Ciunaitis, Wieger Helsdingen, Lasse Landergren, Mateusz Lentner, Jonathan Neeser, Luca Trotta, Marc Naeije   +11 more
openalex   +1 more source

Initial results of the first visible and near-infrared spectrometer on the Martian surface: SuperCam unveils Jezero crater’s ground mineralogy [PDF]

, 2021
Lucia Mandon, Thierry Fouchet, S. Maurice, O. Forni, J. R. Johnson, O. Gasnault, Cathy Quantin‐Nataf, Pierre Beck, Clément Royer, A. Ollila, F. Poulet, C. Pilorget, Pernelle Bernardi, Jean-Michel Réess, Raymond Newell, R. C. Wiens   +15 more
openalex   +1 more source

To Mars through LEO: How commercial space travel will change exploration‐enabling research

Experimental Physiology, EarlyView.
Christopher Puhl, Michail Magkos
wiley   +1 more source

Mars Lander/Rover vehicle development: An advanced space design project for USRA and NASA/OAST [PDF]

A design is proposed for a Mars Lander/Rover (MLR) for use in gathering needed environmental and surface information. The design focus will be upon a Mars Lander/Rover that will leave an orbit around Mars, reenter and soft land on the Martian surface ...

core   +1 more source