2012
DOI: 10.1029/2012ja017780
|View full text |Cite
|
Sign up to set email alerts
|

Spatial distribution of Kelvin‐Helmholtz instability at low‐latitude boundary layer under different solar wind speed conditions

Abstract: Using the PPMLR‐MHD global simulation model, we examined the Kelvin‐Helmholtz (K‐H) instability at the low‐latitude boundary layer (LLBL) under northward interplanetary magnetic field (IMF) conditions with various solar wind speeds (400, 600, and 800 km/s). The spatial distribution of the K‐H wave power in the equatorial plane shows two distinct power populations, referring to the two modes of K‐H surface waves. The spatial evolution of K‐H instability at the boundary layer is classified into four phases: quas… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

9
50
1

Year Published

2013
2013
2018
2018

Publication Types

Select...
9

Relationship

1
8

Authors

Journals

citations
Cited by 44 publications
(60 citation statements)
references
References 51 publications
9
50
1
Order By: Relevance
“…The solar wind dynamic and magnetic pressures are held constant in each simulation run; thus, any surface waves in the LLBL are not generated by magnetic reconnection near the subsolar point or pressure fluctuations of the solar wind. The KHW is sensitive to grid spacing, and a test run using 640×360×360 grid points confirms the reliability of the numerical results [ Li et al , ]. The spatial distribution of KHW power in the equatorial plane are studied for the 400, 600, and 800 runs [ Li et al , ], and here we choose the case of 800 km/s as an example to illustrate the global features of KHW in detail.…”
Section: Methodssupporting
confidence: 58%
“…The solar wind dynamic and magnetic pressures are held constant in each simulation run; thus, any surface waves in the LLBL are not generated by magnetic reconnection near the subsolar point or pressure fluctuations of the solar wind. The KHW is sensitive to grid spacing, and a test run using 640×360×360 grid points confirms the reliability of the numerical results [ Li et al , ]. The spatial distribution of KHW power in the equatorial plane are studied for the 400, 600, and 800 runs [ Li et al , ], and here we choose the case of 800 km/s as an example to illustrate the global features of KHW in detail.…”
Section: Methodssupporting
confidence: 58%
“…The fastest growing wavelengths should be about 10 times greater than boundary layer thicknesses, with wave amplitudes increasing with increasing shears (Walker 1981) and downstream distance (Li et al 2012). The instability is most likely to occur when strong flow shears lie perpendicular to both magnetosheath and magnetospheric magnetic field orientations, a condition most readily obtained on the equatorial flanks of the magnetosphere during intervals of strongly northward or southward IMF orientations (Southwood 1968).…”
Section: Transients At Earth's Magnetopause and In The Cuspsmentioning
confidence: 99%
“…• off the noon meridian (Guo et al 2010;Li et al 2012). The second unstable region starts prior to the terminator and lasts to about −5 R E (meaning that this location is in the anti-sunward direction).…”
Section: Shear Flow Instabilitiesmentioning
confidence: 99%