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The Hohmann-Parker effect measured by the Mars Science Laboratory on the transfer from Earth to Mars: Consequences and opportunities
DOI: 10.1016/j.pss.2013.09.013 Bibcode: 2013P&SS...89..127P

Frahm, R. A.; Wimmer-Schweingruber, R. F.; Christian, E. R. +33 more

We show that a spacecraft launched from Earth towards Mars following a Hohmann minimum energy transfer trajectory has a strong tendency to remain well-connected magnetically to Earth, in the early phase of the transfer, or to Mars in the late phase, via the Parker spiral magnetic field. On the return trip, the spacecraft would remain reasonably we…

2013 Planetary and Space Science
MEx SOHO 20
Redistribution of lunar polar water to mid-latitudes and its role in forming an OH veneer
DOI: 10.1016/j.pss.2013.05.009 Bibcode: 2013P&SS...89...15F

Delory, G. T.; Halekas, J. S.; Farrell, W. M. +4 more

We suggest that energization processes like ion sputtering and impact vaporization can eject/release polar water molecules residing within cold trapped regions with sufficient velocity to allow their redistribution to mid-latitudes. We consider the possibility that these polar-ejected molecules can contribution to the water/OH veneer observed as a…

2013 Planetary and Space Science
Chandrayaan-1 19
Modeling the seasonal variability of the plasma environment in Saturn's magnetosphere between main rings and Mimas
DOI: 10.1016/j.pss.2012.05.001 Bibcode: 2013P&SS...77..126T

Johnson, R. E.; Elrod, M. K.; Tseng, W. -L.

The detection of O2+ and O+ ions over Saturn's main rings by the Cassini INMS and CAPS instruments at Saturn orbit insertion (SOI) in 2004 confirmed the existence of the ring atmosphere and ionosphere. The source mechanism was suggested to be primarily photolytic decomposition of water ice producing neutral O2…

2013 Planetary and Space Science
Cassini 19
Variability in ionospheric total electron content at Mars
DOI: 10.1016/j.pss.2013.08.010 Bibcode: 2013P&SS...86..117M

Withers, Paul; Kofman, Wlodek; Mendillo, Michael +3 more

The Mars Express (MEX) mission includes a multi-purpose radio instrument called the Mars Advanced Radar for Subsurface and Ionospheric Sounding (MARSIS). When used in its ionospheric-penetrating subsurface sounder (SS) radar mode, a by-product of the MARSIS observations is the ray-path-integral of electron densities, called the total electron cont…

2013 Planetary and Space Science
MEx 19
Utility of laser altimeter and stereoscopic terrain models: Application to Martian craters
DOI: 10.1016/j.pss.2013.06.019 Bibcode: 2013P&SS...86...57R

Hynek, Brian M.; Robbins, Stuart J.

The use of numerical datasets of the same type derived from remote sensing instruments is often treated as equivalent in value and utility, within the limits of their spatial resolution. Surface topography is a good example of this. We used gridded digital terrain models (DTMs) derived from both laser altimetry and stereo pairs as well as the orig…

2013 Planetary and Space Science
MEx 19
Nighttime photochemical model and night airglow on Venus
DOI: 10.1016/j.pss.2013.05.022 Bibcode: 2013P&SS...85...78K

Krasnopolsky, Vladimir A.

The photochemical model for the Venus nighttime atmosphere and night airglow (Krasnopolsky, 2010, Icarus 207, 17-27) has been revised to account for the SPICAV detection of the nighttime ozone layer and more detailed spectroscopy and morphology of the OH nightglow. Nighttime chemistry on Venus is induced by fluxes of O, N, H, and Cl with mean hemi…

2013 Planetary and Space Science
VenusExpress 18
Saturn's ULF wave foreshock boundary: Cassini observations
DOI: 10.1016/j.pss.2013.01.014 Bibcode: 2013P&SS...79...64A

Dougherty, M. K.; Mazelle, C.; Bertucci, C. +2 more

Even though the solar wind is highly supersonic, intense ultra-low frequency (ULF) wave activity has been detected in regions just upstream of the bow shocks of magnetized planets. This feature was first observed ahead of the Earth's bow shock, and the corresponding region was called the ULF wave foreshock, which is embedded within the planet's fo…

2013 Planetary and Space Science
Cassini 18
Young viscous flows in the Lowell crater of Orientale basin, Moon: Impact melts or volcanic eruptions?
DOI: 10.1016/j.pss.2013.09.001 Bibcode: 2013P&SS...87...37S

Srivastava, N.; Kumar, D.; Gupta, R. P.

Topographical, morphological and spectral reflectance studies have been carried out for a distinct resurface event inside Copernican aged Lowell crater (13.00°S 103.40°W), Orientale basin, using high resolution TC, MI-VIS, LROC-NAC, and M3 data from Kaguya, Lunar Reconnaissance Orbiter (LRO) and Chandrayaan-1 missions. The resurfacing i…

2013 Planetary and Space Science
Chandrayaan-1 17
Toroidal and poloidal magnetic fields at Venus. Venus Express observations
DOI: 10.1016/j.pss.2012.12.003 Bibcode: 2013P&SS...87...19D

Fedorov, A.; Barabash, S.; Lundin, R. +5 more

Magnetic field and plasma measurements carried out onboard Venus Express during solar minimum conditions suggest the existence of two kinds of magnetic field configuration in the Venusian ionosphere. We interpret these as the manifestation of two different types of generation mechanisms for the induced magnetosphere. A different magnetic field top…

2013 Planetary and Space Science
VenusExpress 16
Solar wind reflection from the lunar surface: The view from far and near
DOI: 10.1016/j.pss.2013.02.004 Bibcode: 2013P&SS...84....1S

Barabash, S.; Wurz, P.; McComas, D. J. +7 more

The Moon appears bright in the sky as a source of energetic neutral atoms (ENAs). These ENAs have recently been imaged over a broad energy range both from near the lunar surface, by India's Chandrayaan-1 mission (CH-1), and from a much more distant Earth orbit by NASA's Interstellar Boundary Explorer (IBEX) satellite. Both sets of observations hav…

2013 Planetary and Space Science
Chandrayaan-1 16