Search Publications

Lava tubes and basaltic caves as astrobiological targets on Earth and Mars: A review
DOI: 10.1016/j.pss.2009.06.004 Bibcode: 2010P&SS...58..592L

Léveillé, Richard J.; Datta, Saugata

Lava tubes and basaltic caves are common features in volcanic terrains on Earth. Lava tubes and cave-like features have also been identified on Mars based on orbital imagery and remote-sensing data. Caves are unique environments where both secondary mineral precipitation and microbial growth are enhanced by stable physico-chemical conditions. Thus…

2010 Planetary and Space Science
MEx 92
Titan's highly dynamic magnetic environment: A systematic survey of Cassini magnetometer observations from flybys TA-T62
DOI: 10.1016/j.pss.2010.04.021 Bibcode: 2010P&SS...58.1230S

Dougherty, Michele K.; Saur, Joachim; Kriegel, Hendrik +5 more

We analyze the variability of the ambient magnetic field near Titan during Cassini encounters TA-T62 (October 2004-October 2009). Cassini magnetometer (MAG) data show that the moon's magnetic environment is strongly affected by its proximity to Saturn's warped and highly dynamic magnetodisk. In the nightside sector of Saturn's magnetosphere, the m…

2010 Planetary and Space Science
Cassini 67
In-flight calibration of the Cassini imaging science sub-system cameras
DOI: 10.1016/j.pss.2010.07.006 Bibcode: 2010P&SS...58.1475W

McEwen, Alfred; Porco, Carolyn; West, Robert +10 more

We describe in-flight calibration of the Cassini Imaging Science Sub-system narrow- and wide-angle cameras using data from 2004 to 2009. We report on the photometric performance of the cameras including the use of polarization filters, point spread functions over a dynamic range greater than 10 7, gain and loss of hot pixels, changes in…

2010 Planetary and Space Science
Cassini eHST 64
Transterminator ion flow in the Martian ionosphere
DOI: 10.1016/j.pss.2010.06.009 Bibcode: 2010P&SS...58.1442F

Fedorov, A.; Barabash, S.; Lundin, R. +4 more

The upper ionospheres of Mars and Venus are permeated by the magnetic fields induced by the solar wind. It is a long-standing question whether these fields can put the dense ionospheric plasma into motion. If so, the transterminator flow of the upper ionosphere could explain a significant part of the ion escape from the planets atmospheres. But it…

2010 Planetary and Space Science
MEx 53
Abundances of Jupiter's trace hydrocarbons from Voyager and Cassini
DOI: 10.1016/j.pss.2010.05.008 Bibcode: 2010P&SS...58.1667N

Zhang, X.; Irwin, P. G. J.; Teanby, N. A. +5 more

The flybys of Jupiter by the Voyager spacecraft in 1979, and over two decades later by Cassini in 2000, have provided us with unique datasets from two different epochs, allowing the investigation of seasonal change in the atmosphere. In this paper we model zonal averages of thermal infrared spectra from the two instruments, Voyager 1 IRIS and Cass…

2010 Planetary and Space Science
Cassini 49
Ismenius Cavus, Mars: A deep paleolake with phyllosilicate deposits
DOI: 10.1016/j.pss.2010.02.005 Bibcode: 2010P&SS...58..941D

Mangold, N.; Le Mouélic, S.; Poulet, F. +2 more

Ismenius Cavus is a basin where several fluvial valleys converge. Three depositional fan deltas are observed at the valleys outlets at similar elevations. These fans suggest long-term fluvial activity accompanied by a lake inside the basin. The elevational difference between the delta plains and the deepest part of the basin floor implies that thi…

2010 Planetary and Space Science
MEx 42
Saturn's magnetospheric interaction with Titan as defined by Cassini encounters T9 and T18: New results
DOI: 10.1016/j.pss.2009.09.017 Bibcode: 2010P&SS...58..327S

Coates, A. J.; Johnson, R. E.; Wahlund, J. -E. +8 more

We present new results of Cassini's T9 flyby with complementary observations from T18. Based on Cassini plasma spectrometer (CAPS) and Cassini magnetometer (MAG), compositional evidence shows the upstream flow for both T9 and T18 appears composed of light ions (H + and H 2+), with external pressures ∼30 times lower…

2010 Planetary and Space Science
Cassini 38
The sunlit lunar atmosphere: A comprehensive study by CHACE on the Moon Impact Probe of Chandrayaan-1
DOI: 10.1016/j.pss.2010.07.027 Bibcode: 2010P&SS...58.1567S

Sridharan, R.; Ahmed, S. M.; Pratim Das, Tirtha +4 more

The altitudinal/latitudinal profile of the lunar atmospheric composition on the sunlit side was unraveled for the first time by the Chandra's Altitudinal Composition Explorer (CHACE) on the Moon Impact Probe, a standalone micro-satellite that impacted at the lunar south pole, as a part of the first Indian mission to Moon, Chandrayaan-1. Systematic…

2010 Planetary and Space Science
Chandrayaan-1 38
The analytic properties of the flapping current sheets in the earth magnetotail
DOI: 10.1016/j.pss.2010.04.016 Bibcode: 2010P&SS...58.1215R

Petrukovich, A. A.; Liu, Z. X.; Rong, Z. J. +2 more

The current sheet in Earth's magnetotail often flaps, and the flapping waves could be induced propagating towards the dawn and dusk flanks, which could make the current sheet dynamic. To explore the dynamic characteristics of current sheet associated with the flapping motion holistically and provide reasonable physical interpretations, detailed di…

2010 Planetary and Space Science
Cluster 37
The Kelvin-Helmholtz instability at Mercury: An assessment
DOI: 10.1016/j.pss.2010.06.008 Bibcode: 2010P&SS...58.1434S

Korth, H.; Blomberg, L. G.; Slavin, J. A. +2 more

The Kelvin-Helmholtz instability is believed to be an important means for the transfer of energy, plasma, and momentum from the solar wind into planetary magnetospheres, with in situ measurements reported from Earth, Saturn, and Venus. During the first MESSENGER flyby of Mercury, three periodic rotations were observed in the magnetic field data po…

2010 Planetary and Space Science
Cluster 36