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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKAN8RW/39RSBBD
Repositorydpi.inpe.br/plutao/2011/06.11.13.53.08
Last Update2011:12.27.15.58.12 (UTC) administrator
Metadata Repositorydpi.inpe.br/plutao/2011/06.11.13.53.09
Metadata Last Update2018:06.05.00.01.21 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.1029/2010JA015913
ISSN0148-0227
2156-2202
Labellattes: 3869820274542343 4 TsurutaniLaVeEcGuNaCo:2011:DiDiFe
Citation KeyTsurutaniLaVeEcGuNaCo:2011:DiDiFe
TitleMagnetosheath and heliosheath mirror mode structures, interplanetary magnetic decreases, and linear magnetic decreases: Differences and distinguishing features
ProjectFAPESP [2007/52533-1]
Year2011
MonthFEB.
Access Date2024, May 17
Secondary TypePRE PI
Number of Files1
Size2159 KiB
2. Context
Author1 Tsurutani, Bruce T.
2 Lakhina, Gurbax S.
3 Verkhoglyadova, Olga P.
4 Echer, Ezequiel
5 Guarnieri, Fernando L.
6 Narita, Yasuhito
7 Constantinescu, Dragos O.
Resume Identifier1
2
3
4 8JMKD3MGP5W/3C9JH3D
Group1
2
3
4 DGE-CEA-INPE-MCT-BR
Affiliation1 Tech Univ Carolo Wilhelmina Braunschweig, Inst Geophys & Extraterr Physik, D-38106 Braunschweig, Germany
2 Indian Inst Geomagnetism, Navi Mumbai 410218, India
3 CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Univ Vale Paraiba, Dept Phys & Astron, BR-12244000 Sao Jose Dos Campos, Brazil
6 Tech Univ Carolo Wilhelmina Braunschweig, Inst Geophys & Extraterr Physik, D-38106 Braunschweig, Germany
7 Tech Univ Carolo Wilhelmina Braunschweig, Inst Geophys & Extraterr Physik, D-38106 Braunschweig, Germany
Author e-Mail Address1
2
3
4 eecher@dge.inpe.br
e-Mail Addresseecher@dge.inpe.br
JournalJournal of Geophysical Research
Volume116
PagesA02103
Secondary MarkB1_ASTRONOMIA_/_FÍSICA B2_CIÊNCIA_DA_COMPUTAÇÃO A1_CIÊNCIAS_AGRÁRIAS_I A1_ECOLOGIA_E_MEIO_AMBIENTE A1_ENGENHARIAS_I A2_ENGENHARIAS_II A1_ENGENHARIAS_III A2_ENGENHARIAS_IV A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR
History (UTC)2011-06-11 17:43:47 :: lattes -> administrator :: 2011
2011-07-19 20:50:10 :: administrator -> marciana :: 2011
2011-11-01 11:21:21 :: marciana -> banon :: 2011
2011-11-18 18:44:26 :: banon -> tereza@sid.inpe.br :: 2011
2011-12-27 15:58:26 :: tereza@sid.inpe.br -> administrator :: 2011
2018-06-05 00:01:21 :: administrator -> tereza@sid.inpe.br :: 2011
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsNONLINEAR ALFVEN WAVES
PLASMA DEPLETION LAYER
TERRESTRIAL BOW SHOCK
SOLAR-WIND PLASMA
EQUATOR-S
ULYSSES OBSERVATIONS
PONDEROMOTIVE FORCE
INTERACTION REGIONS
FIELD OBSERVATIONS
GIACOBINI-ZINNER
AbstractThere has been considerable confusion in the literature about what mirror mode (MM), magnetic decrease (MD), and linear magnetic decrease (LMD) structures are and are not. We will reexamine past spacecraft observations to demonstrate the observational similarities and differences between these magnetic and plasma structures. MM structures in planetary magnetosheaths, cometary sheaths, and the heliosheath have the following characteristics: (1) the structures have little or no changes in the magnetic field direction across the magnetic dips; (2) the structures have quasiperiodic spacings, varying from similar to 20 proton gyroradii (r(p)) in the Earth's magnetosheath to similar to 57 r(p) in the heliosheath; and (3) the magnetic dips have smooth edges. Magnetosheath MM structures are generated by the mirror instability where beta(perpendicular to)/beta(parallel to) > 1 + 1/beta(perpendicular to) (beta is the plasma thermal pressure divided by the magnetic pressure). In general, the sources of free energy for the mirror instability are reasonably well understood: shock compression, field line draping, and, in the cases of comets and the heliosheath, also ion pickup. The observational properties of interplanetary MDs are as follows: (1) there is a broad range of magnetic field angular changes across them; (2) their thicknesses can range from as little as 2-3 r(p) to thousands of r(p), with no "characteristic" size; and (3) they typically are bounded by discontinuities. The mechanism(s) for interplanetary MD generation is (are) currently unresolved, although at least five different mechanisms have been proposed in the literature. Tsurutani et al. (2009a) have argued against mirror instability for those MDs generated within interplanetary corotating interaction regions. Interplanetary LMDs are by definition a subset of MDs with small angular changes across them (theta < 10 degrees). Are LMDs generated by the mirror instability or by another mechanism? Is it possible that there are several different types of LMDs involving different generation mechanisms? At the present time, no one knows the answers to these latter questions.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Magnetosheath and heliosheath...
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5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
Citing Item Listsid.inpe.br/bibdigital/2013/10.01.22.11 2
sid.inpe.br/mtc-m21/2012/07.13.14.45.47 1
DisseminationWEBSCI; AGU; MGA; COMPENDEX.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
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