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The magnetohydrodynamic turbulent cascade in the ecliptic solar wind: Study of Ulysses data
DOI: 10.1016/j.pss.2010.06.005 Bibcode: 2011P&SS...59..592M

Sorriso-Valvo, Luca; Marino, Raffaele; Bruno, Roberto +3 more

The occurrence of a nonlinear turbulent energy cascade in solar wind plasma has been recently established through the observation of an exact law from spacecraft measurements. The main results obtained in the fast, polar wind measured by Ulysses spacecraft are reviewed here. In particular, the turbulent cascade is seen as the mean to provide the e…

2011 Planetary and Space Science
Ulysses 42
State studies of Earth's plasmasphere: A review
DOI: 10.1016/j.pss.2011.03.013 Bibcode: 2011P&SS...59..810S

Singh, A. K.; Singh, R. P.; Siingh, Devendraa

The plasmasphere sandwiched between the ionosphere and the outer magnetosphere is populated by up flow of ionospheric cold (∼1 eV) and dense plasma along geomagnetic field lines. Recent observations from various instruments onboard IMAGE and CLUSTER spacecrafts have made significant advances in our understanding of plasma density irregularities, p…

2011 Planetary and Space Science
Cluster 39
Dynamics and circulation regimes of terrestrial planets
DOI: 10.1016/j.pss.2010.04.024 Bibcode: 2011P&SS...59..900R

Read, P. L.

By the study of simple analogues, either in the form of simplified numerical models or laboratory experiments, considerable insights may be gained as to the likely roles of planetary size, rotation, thermal stratification and other factors in determining the principal length scales, styles of global circulation and dominant waves and instability p…

2011 Planetary and Space Science
VenusExpress 39
Multi-spacecraft study of foreshock cavitons upstream of the quasi-parallel bow shock
DOI: 10.1016/j.pss.2011.02.005 Bibcode: 2011P&SS...59..705K

Kajdič, Primož; Russell, Christopher T.; Blanco-Cano, Xochitl +1 more

In this work we perform the first multi-spacecraft analysis of two foreshock cavitons observed by the Cluster spacecraft. We also study the characteristics of their surrounding regions. Foreshock cavitons are a relatively new type of phenomena in the Earth's foreshock. They appear in regions deep inside the foreshock and are therefore always immer…

2011 Planetary and Space Science
Cluster 36
Retrieval and tentative indentification of the 3 µm spectral feature in Titan's haze
DOI: 10.1016/j.pss.2011.02.002 Bibcode: 2011P&SS...59..699K

Sicardy, B.; Courtin, R.; Sim, C. K. +5 more

Recently, an unidentified 3.3-3.4 µm feature found in the solar occultation spectra of the atmosphere of Titan observed by Cassini/VIMS was tentatively attributed to the C-H stretching mode of aliphatic hydrocarbon chains attached to large organic molecules, but without properly extracting the feature from adjacent influences of strong CH

2011 Planetary and Space Science
Cassini 36
Structured ionospheric outflow during the Cassini T55-T59 Titan flybys
DOI: 10.1016/j.pss.2011.03.007 Bibcode: 2011P&SS...59..788E

Coates, A. J.; Dougherty, M. K.; Wahlund, J. -E. +7 more

During the final three of the five consecutive and similar Cassini Titan flybys T55-T59 we observe a region characterized by high plasma densities (electron densities of 1-8 cm-3) in the tail/nightside of Titan. This region is observed progressively farther downtail from pass to pass and is interpreted as a plume of ionospheric plasma e…

2011 Planetary and Space Science
Cassini 33
Comparative study of ion cyclotron waves at Mars, Venus and Earth
DOI: 10.1016/j.pss.2010.01.004 Bibcode: 2011P&SS...59.1039W

Russell, C. T.; Wei, H. Y.; Zhang, T. L. +1 more

Ion cyclotron waves are generated in the solar wind when it picks up freshly ionized planetary exospheric ions. These waves grow from the free energy of the highly anisotropic distribution of fresh pickup ions, and are observed in the spacecraft frame with left-handed polarization and a wave frequency near the ion's gyrofrequency. At Mars and Venu…

2011 Planetary and Space Science
VenusExpress 32
Observations of water vapour and carbon monoxide in the Martian atmosphere with the SWC of PFS/MEX
DOI: 10.1016/j.pss.2010.12.006 Bibcode: 2011P&SS...59..149S

Sindoni, G.; Geminale, A.; Formisano, V.

In the history of Mars exploration its atmosphere and planetary climatology aroused particular interest. In the study of the minor gases abundance in the Martian atmosphere, water vapour became especially important, both because it is the most variable trace gas, and because it is involved in several processes characterizing the planetary atmosphe…

2011 Planetary and Space Science
MEx 32
Little variability of methane on Mars induced by adsorption in the regolith
DOI: 10.1016/j.pss.2010.09.022 Bibcode: 2011P&SS...59..247M

Forget, F.; Lefèvre, F.; Gough, R. +1 more

The mechanisms that can induce short term variations of methane in the Martian atmosphere, and thus explain the observations currently available, are yet to be discovered. Seasonal exchange with the regolith, caused by reversible adsorption, is expected to induce both spatial and time variabilities without the need for additional sources and sinks…

2011 Planetary and Space Science
MEx 24
Sulfuric acid aerosols in the atmospheres of the terrestrial planets
DOI: 10.1016/j.pss.2010.05.020 Bibcode: 2011P&SS...59..934M

Grinspoon, David H.; Toon, Owen B.; McGouldrick, Kevin

Clouds and hazes composed of sulfuric acid are observed to exist or postulated to have once existed on each of the terrestrial planets with atmospheres in our solar system. Venus today maintains a global cover of clouds composed of a sulfuric acid/water solution that extends in altitude from roughly 50 km to roughly 80 km. Terrestrial polar strato…

2011 Planetary and Space Science
VenusExpress 24