2009
DOI: 10.5194/angeo-27-1353-2009
|View full text |Cite
|
Sign up to set email alerts
|

Kinetic thin current sheets: their formation in relation to magnetotail mesoscale turbulent dynamics

Abstract: Abstract. Dynamics of the magnetotail plasma sheet (PS) features nonlinear structures on two totally different scales. There are very thin current sheets (CS) on kinetic scale of the ion gyroradius. And there are intense plasma flow and magnetic field variations on mesoscales (a few earth radii); those are interpreted as mostly 2-D MHD turbulence. On the other hand, the specific nature of slow large scale magnetotail evolution leads to large differences in the PS properties and those of the lobe plasma. As a r… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
2
0

Year Published

2014
2014
2021
2021

Publication Types

Select...
7

Relationship

1
6

Authors

Journals

citations
Cited by 8 publications
(2 citation statements)
references
References 18 publications
(26 reference statements)
0
2
0
Order By: Relevance
“…Outside the diffusion region, the process of "magnetic annihilation" -the transformation of electromagnetic energy into the energy of plasma flows, meaning magnetic reconnection in the wider sense, is determined by ion motions, including those that are substantially nonadiabatic in thin layers adjacent to the diffusion region. As was pointed out in Domrin and Kropotkin (2007a, b, c), Kropotkin and Domrin (2009), and Kropotkin (2013), in that region the process is dominated by an "anisotropic" CS, the structure of which is determined by the specific ion orbits. This leads to ion anisotropy of a certain type, dependent on the distance from the central plane.…”
Section: Introductionmentioning
confidence: 73%
“…Outside the diffusion region, the process of "magnetic annihilation" -the transformation of electromagnetic energy into the energy of plasma flows, meaning magnetic reconnection in the wider sense, is determined by ion motions, including those that are substantially nonadiabatic in thin layers adjacent to the diffusion region. As was pointed out in Domrin and Kropotkin (2007a, b, c), Kropotkin and Domrin (2009), and Kropotkin (2013), in that region the process is dominated by an "anisotropic" CS, the structure of which is determined by the specific ion orbits. This leads to ion anisotropy of a certain type, dependent on the distance from the central plane.…”
Section: Introductionmentioning
confidence: 73%
“…¬ÂÍ ËÊÄÇÔÕÐÑ, ÒÑAEÑÃÐÞÇ ÕÑÍÑÄÞÇ ÑÃÓÂÊÑÄÂÐËâ, ÑÃÇÔÒÇÚËÄÂáÜËÇ AEÎËÕÇÎßÐÑÇ ÔÖÜÇÔÕÄÑÄÂÐËÇ ÍÄÂÊËÔÕÂ-ÙËÑÐÂÓÐÑÅÑ ÏÂÅÐËÕÐÑÅÑ ÒÑÎâ Ä ÃÇÔÔÕÑÎÍÐÑÄËÕÇÎßÐÑÌ ÐÇ-ÓÂÄÐÑÄÇÔÐÑÌ ÒÎÂÊÏÇ, ÄÂÉÐÞ AEÎâ ÑÒËÔÂÐËâ ÍÓÖÒÐÑÏÂÔÛ-ÕÂÃÐÞØ ÓÇÅÖÎâÓÐÞØ ÔÕÓÖÍÕÖÓ (ÐÂÒÓËÏÇÓ, ÕÑÍÑÄÞØ ÔÎÑÈÄ Ä ÏÂÅÐËÕÑÔ×ÇÓÇ ©ÇÏÎË [34,45], Р³ÑÎÐÙÇ [47], Ä àÍÄÂÕÑÓË-ÂÎßÐÑÌ ÑÃÎÂÔÕË ÏÂÅÐËÕÑÔ×ÇÓ ÐÇÌÕÓÑÐÐÞØ ÊÄÈÊAE Ô ÒÖÎß-ÔÂÓÐÞÏ ÄÇÕÓÑÏ [57,58]) Ë ÏÇÎÍÑÏÂÔÛÕÂÃÐÞØ ÕÖÓÃÖÎÇÐÕ-ÐÞØ ÔÕÓÖÍÕÖÓ (ÐÂÒÓËÏÇÓ, ØÂÑÕËÚÇÔÍËØ ÕÑÍÑÄÞØ ÑÃÓÂÊÑÄÂ-ÐËÌ Ä ÕÖÓÃÖÎÇÐÕÐÑÌ ÚÂÔÕË ÕÑÍÑÄÑÅÑ ÔÎÑâ ÊÇÏÐÑÌ ÏÂÅ-ÐËÕÑÔ×ÇÓÞ [59] Ë ÕÑÍÑÄÞØ ×ËÎÂÏÇÐÕÑÄ Ä ÒÎÂÊÏÇÐÐÞØ AEÉÇÕÂØ ËÎË Ä ÑÍÓÇÔÕÐÑÔÕË ×ÓÑÐÕ ÃÇÔÔÕÑÎÍÐÑÄËÕÇÎßÐÞØ ÖAEÂÓÐÞØ ÄÑÎÐ [51,53,54,60] [70,74,82]). …”
mentioning
confidence: 99%