Connection Between Foreshock Structures and the Generation of Magnetosheath Jets: Vlasiator Results
Earth’s magnetosheath consists of shocked solar wind plasma that has been compressed and slowed down at the Earth’s bow shock. Magnetosheath jets are pulses of enhanced dynamic pressure in the magnetosheath. Jets have been observed by numerous spacecraft
Jonas Suni, M Palmroth, Lucile Turc
exaly +2 more sources
First identification of mirror mode waves in Venus' magnetosheath?
In this paper first time observations of mirror mode like structures in Venus' magnetosheath are presented. Using magnetometer data from the Venus Express spacecraft it is shown that in two regions in the Venusian magnetosheath strong compressional waves
M Volwerk, T L Zhang, M Delva
exaly +2 more sources
Plasma and Magnetic Field Turbulence in the Earth’s Magnetosheath at Ion Scales
Crossing the Earth’s bow shock is known to crucially affect solar wind plasma including changes in turbulent cascade. The present review summarizes results of more than 15 years of experimental exploration into magnetosheath turbulence.
L S Rakhmanova +2 more
exaly +3 more sources
Honeycomb‐Like Magnetosheath Structure Formed by Jets: Three‐Dimensional Global Hybrid Simulations
Magnetosheath jets with enhanced dynamic pressure are common in the Earth's magnetosheath. They can impact the magnetopause, causing deformation of the magnetopause. Here we investigate the 3‐D structure of magnetosheath jets using a realistic‐scale, 3‐D
Junyi Ren, Jin Guo, Quanming Lu
exaly +2 more sources
THEMIS Observations of Particle Acceleration by a Magnetosheath Jet‐Driven Bow Wave
Localized magnetosheath jets with high dynamic pressure are frequently observed downstream of Earth's bow shock. When such a fast magnetosheath jet compresses the ambient magnetosheath plasma, an earthward compressional bow wave could form.
Terry Z Liu, H Hietala, V Angelopoulos
exaly +2 more sources
On the Kinetic Energy Input of Magnetosheath Jets Into the Magnetosheath
Magnetosheath jets, plasma structures with enhanced dynamic pressure, are frequently observed in the terrestrial magnetosheath. However, their mass, momentum, and energy content are still unknown. We utilize Amitis, a 3D hybrid‐kinetic plasma simulation,
E Kramer, S Fatemi, M Hamrin
exaly +2 more sources
Correlation length of magnetosheath fluctuations: Cluster statistics [PDF]
Magnetosheath parameters are usually described by gasdynamic or magnetohydrodynamic (MHD) models but these models cannot account for one of the most important sources of magnetosheath fluctuations – the foreshock.
O. Gutynska +2 more
doaj +1 more source
Magnetosheath plasma flow model around Mercury [PDF]
The magnetosheath is defined as the plasma region between the bow shock, where the super-magnetosonic solar wind plasma is decelerated and heated, and the outer boundary of the intrinsic planetary magnetic field, the so-called magnetopause.
D. Schmid +5 more
doaj +1 more source
Magnetosheath cavities: case studies using Cluster observations [PDF]
This paper presents examples of magnetosheath cavities in Cluster spacecraft observations. The cavities are accompanied by high energy particles in the magnetosheath and characterized by depressed magnetic fields and densities.
F. T. Katırcıoğlu +5 more
doaj +1 more source
The Earth's magnetosheath: Structures, waves and turbulence
When the solar wind encounters the blunt Earth's magnetosphere, a detached shock (i.e., the bow shock) forms at a distance about ten Earth radii from the Earth.
Shiyong Huang
doaj +1 more source

