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Correction to 'Plasma environment of Venus: Comparison of Venus Express ASPERA‐4 measurements with 3‐D hybrid simulations'
- Source :
- Journal of Geophysical Research. 114
- Publication Year :
- 2009
- Publisher :
- American Geophysical Union (AGU), 2009.
-
Abstract
- Figure 9. Simulation results in the terminator plane, i.e., looking from behind on Venus. The solar wind is orientated out of the plane (+x axis), the convective electric field is antiparallel to the (+z) axis and points away from the planet; thus, the background magnetic field completes the right-handed system (+y axis). Figure 10 displays (left) the solar wind density (nsw), (middle) the heavy ion density (nhi), and (right) the background magnetic field. An asymmetric bow shock, exhibiting a shocklet structure, is formed in front of the obstacle owing to the supersonic solar wind (left plot). The interplanetary magnetic field is draping around Venus generating an induced magnetotail on the nightside of the planet (right plot). See text for details. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, E00B98, doi:10.1029/2009JE003377, 2009
- Subjects :
- Atmospheric Science
Soil Science
Venus
Astrophysics
Aquatic Science
Oceanography
Geochemistry and Petrology
Planet
Electric field
Earth and Planetary Sciences (miscellaneous)
Interplanetary magnetic field
Earth-Surface Processes
Water Science and Technology
Physics
Ecology
biology
Paleontology
Forestry
Geophysics
Plasma
biology.organism_classification
Bow shocks in astrophysics
Magnetic field
Solar wind
Space and Planetary Science
Subjects
Details
- ISSN :
- 01480227
- Volume :
- 114
- Database :
- OpenAIRE
- Journal :
- Journal of Geophysical Research
- Accession number :
- edsair.doi...........86cf1947f098ecf11132d75f5f98f804
- Full Text :
- https://doi.org/10.1029/2009je003377