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Statements

Subject Item
n2:RIV%2F68378289%3A_____%2F12%3A00378032%21RIV13-AV0-68378289
rdf:type
skos:Concept n12:Vysledek
dcterms:description
The magnetosheath is occupied with a variety of low-frequency fluctuations from different sources. Among them, the bow shock and dominantly foreshock processes are often considered as their major contributors. We use distant (Wind) and close (Geotail) interplanetary magnetic field monitors and compare their measurements with simultaneous magnetic field observations within the dawn (Time History of Events and Macroscale Interactions During Substorms (THEMIS)) and dusk (Cluster) magnetosheath. We have found that coherent low-frequency (10(-4)-10(-3) Hz) variations can be registered in all locations; thus, their source is in the solar wind. On the other hand, no correlation was found for fluctuations of higher frequencies (up to 10(-1) Hz); therefore, these fluctuations should be generated by local sources. We suggest that one of these sources is connected with magnetopause processes because the fluctuation amplitude grows toward the magnetopause. The magnetosheath is occupied with a variety of low-frequency fluctuations from different sources. Among them, the bow shock and dominantly foreshock processes are often considered as their major contributors. We use distant (Wind) and close (Geotail) interplanetary magnetic field monitors and compare their measurements with simultaneous magnetic field observations within the dawn (Time History of Events and Macroscale Interactions During Substorms (THEMIS)) and dusk (Cluster) magnetosheath. We have found that coherent low-frequency (10(-4)-10(-3) Hz) variations can be registered in all locations; thus, their source is in the solar wind. On the other hand, no correlation was found for fluctuations of higher frequencies (up to 10(-1) Hz); therefore, these fluctuations should be generated by local sources. We suggest that one of these sources is connected with magnetopause processes because the fluctuation amplitude grows toward the magnetopause.
dcterms:title
Multipoint study of magnetosheath magnetic field fluctuations and their relation to the foreshock Multipoint study of magnetosheath magnetic field fluctuations and their relation to the foreshock
skos:prefLabel
Multipoint study of magnetosheath magnetic field fluctuations and their relation to the foreshock Multipoint study of magnetosheath magnetic field fluctuations and their relation to the foreshock
skos:notation
RIV/68378289:_____/12:00378032!RIV13-AV0-68378289
n12:predkladatel
n13:ico%3A68378289
n3:aktivita
n9:I n9:S n9:P n9:Z
n3:aktivity
I, P(GA205/09/0112), P(GA205/09/0170), P(ME09106), S, Z(MSM0021620860)
n3:cisloPeriodika
A4
n3:dodaniDat
n10:2013
n3:domaciTvurceVysledku
n19:8419329
n3:druhVysledku
n11:J
n3:duvernostUdaju
n15:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
152454
n3:idVysledku
RIV/68378289:_____/12:00378032
n3:jazykVysledku
n20:eng
n3:klicovaSlova
magnetosheath; magnetopause and boundary layers; correlation analysis; spectral analysis
n3:klicoveSlovo
n17:magnetosheath n17:correlation%20analysis n17:spectral%20analysis n17:magnetopause%20and%20boundary%20layers
n3:kodStatuVydavatele
US - Spojené státy americké
n3:kontrolniKodProRIV
[8ADF12570024]
n3:nazevZdroje
Journal of Geophysical Research
n3:obor
n18:BL
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:projekt
n8:GA205%2F09%2F0112 n8:GA205%2F09%2F0170 n8:ME09106
n3:rokUplatneniVysledku
n10:2012
n3:svazekPeriodika
117
n3:tvurceVysledku
Přech, L. Němeček, Z. Šimůnek, Jiří Šafránková, J. Gutynska, O.
n3:wos
000302872600001
n3:zamer
n4:MSM0021620860
s:issn
0148-0227
s:numberOfPages
12
n16:doi
10.1029/2011JA017240