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Titan's plasma environment: 3D hybrid kinetic modeling of the TA flyby and comparison with CAPS-ELS and RPWS LP observations
DOI: 10.1016/j.pss.2014.02.012 Bibcode: 2014P&SS...93..119L

Hartle, R. E.; Sittler, E. C.; Cooper, J. F. +2 more

In this report we discuss the global plasma environment of the TA flyby from the perspective of 3D hybrid modeling. In our model the background, pickup, and ionospheric ions are considered as particles, whereas the electrons are described as a fluid. Inhomogeneous photoionization, electron-impact ionization and charge exchange are included in our …

2014 Planetary and Space Science
Cassini 4
Dust Impact Monitor (DIM) onboard Rosetta/Philae: Tests with ice particles as comet analog materials
DOI: 10.1016/j.pss.2014.05.014 Bibcode: 2014P&SS...99..128F

Flandes, Alberto; Krüger, Harald; Loose, Alexander +2 more

In 2014 the European Space Agency's spacecraft Rosetta will encounter the short-period comet 67P/Churyumov-Gerasimenko. Rosetta carries the lander spacecraft Philae on board which will attempt to land on the comet's nucleus. Amongst Philae's instruments, the Dust Impact Monitor (DIM) using piezoelectric sensors is aimed at measuring the physical p…

2014 Planetary and Space Science
Rosetta 4
Amazonian thermokarst in Danielson crater, Arabia Terra region, Mars
DOI: 10.1016/j.pss.2014.09.006 Bibcode: 2014P&SS..104..310B

Baioni, Davide; Murana, Alessio; Tramontana, Mario

This paper describe the possible ice-related landforms observed within Danielson crater which is centered at about 8°N and 353°E, in the region of southwestern Arabia Terra about 800 km south of Becquerel crater.

A morphological survey of the study area through an analysis of the available Mars images was performed. The features of the landfo…

2014 Planetary and Space Science
MEx 3
Radio emission from dusty galaxies observed by AKARI
DOI: 10.1016/j.pss.2014.03.016 Bibcode: 2014P&SS..100...12P

Takeuchi, T. T.; Pollo, A.; Solarz, A. +2 more

We probe radio-infrared correlation for two samples of extragalactic sources from the local Universe from the AKARI All-Sky Catalogue. The first, smaller sample (1053 objects) was constructed by the cross-correlation of the AKARI/FIS All-Sky Survey Bright Source Catalogue, the AKARI IRC All-Sky Survey Point Source Catalogue and the NRAO VLA Sky Su…

2014 Planetary and Space Science
AKARI 3
Radar investigations of Apollinaris Mons on Mars: Exploring the origin of the fan deposits
DOI: 10.1016/j.pss.2014.09.007 Bibcode: 2014P&SS..103..262E

El-Maarry, M. R.; Heggy, E.; Dohm, J. M.

Apollinaris Mons is an isolated volcano on Mars straddling the boundary between the southern highlands and the northern plains. One of its most distinctive features is its massive fan-shaped deposit that extends from a breach on its summit to distances of more than 150 km and drapes its entire southern flank. The composition and formation mechanis…

2014 Planetary and Space Science
MEx 3
Calibrating Mars Orbiter Laser Altimeter pulse widths at Mars Science Laboratory candidate landing sites
DOI: 10.1016/j.pss.2014.05.012 Bibcode: 2014P&SS...99..118P

Muller, Jan-Peter; Grindrod, Peter M.; Gupta, Sanjeev +1 more

Accurate estimates of surface roughness allow quantitative comparisons between planetary terrains. These comparisons enable us to improve our understanding of commonly occurring surface processes, and develop a more complete analysis of candidate landing and roving sites. A (secondary) science goal of the Mars Orbiter Laser Altimeter was to map su…

2014 Planetary and Space Science
MEx 2
Three predictions: Comet 67P/Churyumov-Gerasimenko, comet C/2012 K1 PANSTARRS, and comet C/2013 V5 Oukaimeden
DOI: 10.1016/j.pss.2014.05.005 Bibcode: 2014P&SS...99..171F

Ferrín, Ignacio

We make the following predictions: (1) The secular light curve (SLC) of comet 67P/Churyumov-Gerasimenko exhibits a photometric anomaly in magnitude that is present in 1982, 1996, 2002 and 2009. Thus it must be real. We interpret this anomaly as a topographic feature on the surface of the nucleus that may be a field of debris, a region made only of…

2014 Planetary and Space Science
Rosetta 2
Corrigendum to “Evolution of Titan's major atmospheric gases and cooling since accretion” [Planet. Space Sci. 93-94 (2014) 41-53]
DOI: 10.1016/j.pss.2014.07.005 Bibcode: 2014P&SS..101..210G

Gilliam, Ashley E.; Lerman, Abraham

2014 Planetary and Space Science
Cassini 2
Deriving the characteristics of warm electrons (100-500 eV) in the magnetosphere of Saturn with the Cassini Langmuir probe
DOI: 10.1016/j.pss.2014.09.008 Bibcode: 2014P&SS..104..173G

Schippers, P.; Gurnett, D. A.; Lewis, G. R. +6 more

Though Langmuir probes (LP) are designed to investigate cold plasma regions (e.g. ionospheres), a recent analysis revealed a strong sensitivity of the Cassini LP measurements to hundreds of eV electrons. These warm electrons impact the surface of the probe and generate a significant current of secondary electrons, that impacts both the DC level an…

2014 Planetary and Space Science
Cassini 1
Toward a numerical deshaker for PFS
DOI: 10.1016/j.pss.2013.11.012 Bibcode: 2014P&SS...91...45S

Kowalski, M.; Schmidt, F.; Giuranna, M. +3 more

The Planetary Fourier Spectrometer (PFS) onboard Mars Express (MEx) is the instrument with the highest spectral resolution observing Mars from orbit since January 2004. It permits studying the atmospheric structure, major and minor compounds. The present time version of the calibration is limited by the effects of mechanical vibration, currently n…

2014 Planetary and Space Science
MEx 0