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Disappearing induced magnetosphere at Venus: Implications for close-in exoplanets
DOI: 10.1029/2009GL040515 Bibcode: 2009GeoRL..3620203Z

Russell, C. T.; Lammer, H.; Zhang, T. L. +4 more

The solar wind interaction with a planetary atmosphere produces a magnetosphere-like structure near the planet whether or not the planet has an intrinsic global magnetic field. In the case of planets like Venus or Mars, which have no global intrinsic magnetic field but possess a significant atmosphere, a magnetosphere is induced in the highly cond…

2009 Geophysical Research Letters
VenusExpress 44
MESSENGER and Venus Express observations of the solar wind interaction with Venus
DOI: 10.1029/2009GL037876 Bibcode: 2009GeoRL..36.9106S

Barabash, Stas; Zhang, Tielong; Boardsen, Scott A. +15 more

At 23:08 UTC on 5 June 2007 the MESSENGER spacecraft reached its closest approach altitude of 338 km during its final flyby of Venus en route to its 2011 orbit insertion at Mercury. The availability of the simultaneous Venus Express solar wind and interplanetary magnetic field measurements provides a rare opportunity to examine the influence of up…

2009 Geophysical Research Letters
VenusExpress 38
Giant vortices lead to ion escape from Venus and re-distribution of plasma in the ionosphere
DOI: 10.1029/2008GL036977 Bibcode: 2009GeoRL..36.7202P

Barabash, S.; Zhang, T. L.; Balikhin, M. A. +3 more

The interaction of the solar wind with Venus has a significant influence on the evolution of its atmosphere. Due to the lack of an intrinsic planetary magnetic field, there is direct contact between the fast flowing solar wind and the Venusian ionosphere. This leads to a number of different types of atmospheric escape process. Using Venus Express …

2009 Geophysical Research Letters
VenusExpress 35
A sporadic layer in the Venus lower ionosphere of meteoric origin
DOI: 10.1029/2008GL035875 Bibcode: 2009GeoRL..36.5203P

Pätzold, M.; Christou, A. A.; Bird, M. K. +4 more

The Venus Express Radio Science (VeRa) experiment aboard Venus Express has detected, by means of radio occultation, distinct, low-lying layers of electron density below the base (115 km altitude) of the ionosphere of Venus. A plausible origin of these lowest layers is ionization by the influx of meteoroids into the atmosphere. The layers appeared …

2009 Geophysical Research Letters
VenusExpress 34
On the elusive hot oxygen corona of Venus
DOI: 10.1029/2009GL037575 Bibcode: 2009GeoRL..3610204L

Lammer, H.; Shematovich, V. I.; Lichtenegger, H. I. M. +2 more

After more than two years in orbit still no Venus Express observations were published concerning the hot oxygen corona of Venus which could verify the corresponding controversial observations of Venera 11 and PVO, three decades ago. Based on recent energy and mass dependent collision cross sections, the energy distributions of hot atomic oxygen cr…

2009 Geophysical Research Letters
VenusExpress 29
Vortex circulation on Venus: Dynamical similarities with terrestrial hurricanes
DOI: 10.1029/2008GL036093 Bibcode: 2009GeoRL..36.4204L

Piccioni, Giuseppe; Markiewicz, Wojciech J.; Limaye, Sanjay S. +3 more

Some dynamical and morphological similarities exist between the vortex organization of the atmosphere in the northern and southern hemispheres of Venus and the tropical cyclones/hurricanes on Earth. An S-shape feature detected in the center of the vortices on Venus from Pioneer Venus Orbiter and Venus Express observations has also been seen in tro…

2009 Geophysical Research Letters
VenusExpress 27
Hydrogen in the extended Venus exosphere
DOI: 10.1029/2008GL036164 Bibcode: 2009GeoRL..36.1203D

Zhang, T. L.; Volwerk, M.; Bertaux, J. L. +4 more

The nearly absence of water in the atmosphere of Venus is a major difference to the situation at Earth. The actual content of hydrogen in the exosphere is still an open issue, since no in situ measurements are available yet. A different method uses the presence of proton cyclotron waves as an early tracer of ionized planetary hydrogen picked-up by…

2009 Geophysical Research Letters
VenusExpress 20
Magnetosheath fluctuations at Venus for two extreme orientations of the interplanetary magnetic field
DOI: 10.1029/2009GL037725 Bibcode: 2009GeoRL..36.9102D

Zhang, T. L.; Wang, C.; Baumjohann, W. +3 more

Using the magnetosheath crossings of Venus Express on two consecutive days, we investigate magnetic fluctuations in the same locations for two extreme interplanetary magnetic field orientations, i.e., nearly along and nearly perpendicular to the solar wind flow. It is shown that the properties of the fluctuations are drastically different at basic…

2009 Geophysical Research Letters
VenusExpress 14
Modeling the response of the induced magnetosphere of Venus to changing IMF direction using MESSENGER and Venus Express observations
DOI: 10.1029/2008GL036718 Bibcode: 2009GeoRL..36.4109B

Boardsen, Scott A.; Gloeckler, George; Ho, George C. +14 more

The second MESSENGER flyby of Venus on 5 June 2007 provided a new opportunity to study the response of the induced magnetosphere of the planet to changes in the direction of the interplanetary magnetic field (IMF). At the time of the MESSENGER flyby, the European Space Agency's Venus Express spacecraft was located outside the magnetosphere and pro…

2009 Geophysical Research Letters
VenusExpress 8
Tsallis distribution of the interplanetary magnetic field at 0.72 AU: Venus Express observation
DOI: 10.1029/2009GL038395 Bibcode: 2009GeoRL..3611103L

Zhang, T. L.; Wang, C.; Li, X. Y.

Previous work shows that Probability Distribution Functions (PDFs) of the interplanetary magnetic field strength differences can be described by a single function - Tsallis distribution at Earth and beyond. Launch of Venus Express enables us to extend the application of Tsallis distribution to the inner heliosphere at 0.72 AU. This paper analyzes …

2009 Geophysical Research Letters
VenusExpress 0