2016
DOI: 10.3847/0004-637x/818/1/66
|View full text |Cite
|
Sign up to set email alerts
|

Influence of the Nonlinearity Parameter on the Solar Wind Sub-Ion Magnetic Energy Spectrum: Flr–landau Fluid Simulations

Abstract: The cascade of kinetic Alfvén waves (KAWs) at the sub-ion scales in the solar wind is numerically simulated using a fluid approach that retains ion and electron Landau damping, together with ion finite Larmor radius corrections. Assuming initially equal and isotropic ion and electron temperatures, and an ion beta equal to unity, different simulations are performed by varying the propagation direction and the amplitude of KAWs that are randomly driven at a transverse scale of about one fifth of the proton gyror… Show more

Help me understand this report
View preprint versions

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
34
0

Year Published

2016
2016
2024
2024

Publication Types

Select...
9

Relationship

3
6

Authors

Journals

citations
Cited by 33 publications
(34 citation statements)
references
References 45 publications
(48 reference statements)
0
34
0
Order By: Relevance
“…These exponents are to be compared with satellite observational data that display slopes steeper than the WWs −11/3 spectrum. Note that other physical effects such as Landau damping Sulem et al 2016)) and intermittency corrections associated with coherent structures, such as current sheets (Boldyrev et al 2013), can also lead to steeper spectra. It should be stressed that both phenomenological arguments and numerical simulations predict a transition at d e , while observational spectra in the terrestrial magnetosheath only display a transition at ρ e (Huang et al 2014), associated with electron demagnetization.…”
Section: Resultsmentioning
confidence: 99%
“…These exponents are to be compared with satellite observational data that display slopes steeper than the WWs −11/3 spectrum. Note that other physical effects such as Landau damping Sulem et al 2016)) and intermittency corrections associated with coherent structures, such as current sheets (Boldyrev et al 2013), can also lead to steeper spectra. It should be stressed that both phenomenological arguments and numerical simulations predict a transition at d e , while observational spectra in the terrestrial magnetosheath only display a transition at ρ e (Huang et al 2014), associated with electron demagnetization.…”
Section: Resultsmentioning
confidence: 99%
“…In these approaches, we observe a transition near the ion scales with a steepening in the magnetic field power and a simultaneous flattening in the electric field power fluctuations (Matthaeus et al 2008). Steeper spectra, as observed in the solar wind and in magnetospheres, have been often reproduced by the use of both 2D (Franci et al 2015b(Franci et al ,a, 2016b and 3D (see, e.g., Howes et al 2011;Franci et al 2018b) kinetics models, as well as in fluid models that include kinetic dissipative effects like the ion and electron Landau damping (Sulem et al 2016). It has been thus suggested than the steepening of the spectra is strictly correlated to deformations in the particle's velocity distribution function associated, for example, to wave-particle interactions such as instabilities and wave damping, to thermal anisotropies, and/or to non gyrotropic terms in the full pressure tensor (Del Sarto et al 2016;Del Sarto & Pegoraro 2018) that can drive dissipative effects (Yang et al 2017a).…”
Section: Introductionmentioning
confidence: 99%
“…In order to investigate such complex dynamics, several analytical [11-16, 23, 24] and numerical [25][26][27][28][29][30][31][32][33][34][35][36][37][38][39][40][41] studies have been presented over the last few years. So far numerical studies have been performed mainly within a decaying turbulence framework, while a continuous forcing mechanism permits reaching a 'quasi-steady turbulent regime' over which the statistics of the performed analysis can be improved.…”
Section: Introductionmentioning
confidence: 99%