Propagation Characteristics of Whistler-Mode Chorus during Geomagnetic Activities

A recently introduced ray-tracing method is adopted to study the propagation characteristics of whistler-mode chorus during different geomagnetic activities by using a global core plasma density model. Numerical calculations show that chorus waves tend to settle on a preferable magnetic shell L in t...

Full description

Saved in:
Bibliographic Details
Published inChinese physics letters Vol. 27; no. 5; pp. 170 - 173
Main Author 周庆华 贺艺华 何兆国 杨昶
Format Journal Article
LanguageEnglish
Published IOP Publishing 01.05.2010
Subjects
Online AccessGet full text
ISSN0256-307X
1741-3540
DOI10.1088/0256-307x/27/5/055204

Cover

Loading…
Abstract A recently introduced ray-tracing method is adopted to study the propagation characteristics of whistler-mode chorus during different geomagnetic activities by using a global core plasma density model. Numerical calculations show that chorus waves tend to settle on a preferable magnetic shell L in the vicinity of the plasmapause. During high geomagnetic activity, the plasmapause position moves inward close to the Earth and chorus trajectories move inward together with plasmapause. The trajectory move closer to the plasmapause as θ increases. Chorus wave with lower frequencies will reflect multiple times while chorus wave with higher frequencies reflect once at the plasmapause before settling on the vicinity of the plasmapause. The current results present a first detailed study on the propagation characteristics of chorus during geomagnetic activities, and may account for the observation that chorus tends to be present in the vicinity of the plasmapause.
AbstractList A recently introduced ray-tracing method is adopted to study the propagation characteristics of whistler-mode chorus during different geomagnetic activities by using a global core plasma density model. Numerical calculations show that chorus waves tend to settle on a preferable magnetic shell L in the vicinity of the plasmapause. During high geomagnetic activity, the plasmapause position moves inward close to the Earth and chorus trajectories move inward together with plasmapause. The trajectory move closer to the plasmapause as 9 increases. Chorus wave with lower frequencies will reflect multiple times while chorus wave with higher frequencies reflect once at the plasmapause before settling on the vicinity of the plasmapause. The current results present a first detailed study on the propagation characteristics of chorus during geomagnetic activities, and may account for the observation that chorus tends to be present in the vicinity of the plasmapause.
A recently introduced ray-tracing method is adopted to study the propagation characteristics of whistler-mode chorus during different geomagnetic activities by using a global core plasma density model. Numerical calculations show that chorus waves tend to settle on a preferable magnetic shell L in the vicinity of the plasmapause. During high geomagnetic activity, the plasmapause position moves inward close to the Earth and chorus trajectories move inward together with plasmapause. The trajectory move closer to the plasmapause as θ increases. Chorus wave with lower frequencies will reflect multiple times while chorus wave with higher frequencies reflect once at the plasmapause before settling on the vicinity of the plasmapause. The current results present a first detailed study on the propagation characteristics of chorus during geomagnetic activities, and may account for the observation that chorus tends to be present in the vicinity of the plasmapause.
Author 周庆华 贺艺华 何兆国 杨昶
AuthorAffiliation School of Physics and Electronic Sciences, Changsha University of Science and Technology, Changsha 410004 State Key Laboratory of Space Weather, Chinese Academy of Sciences, Beijing 100190
Author_xml – sequence: 1
  fullname: 周庆华 贺艺华 何兆国 杨昶
BookMark eNqNkUFLwzAYQINMcJv-BKF48WJd0jRtiqcxdAoTFRS9hSz9ukW7pksy0X9v5uZFBT3lO7yXL7z0UKcxDSB0SPApwZwPcMKymOL8bZDkAzbAjCU43UFdkqckpizFHdT9Yp72UM-5Z4wJ4YR00d2tNa2cSa9NE43m0krlwWrntXKRqaLHeZhrsPG1KSEAxq5cVK6sbmbRGMxCzhoIbDRUXr9qr8Hto91K1g4OtmcfPVyc348u48nN-Go0nMQqZZmPy4KrEk8zgCrPIS0gmVJGgRRJyRPAJTBcYE45raQECmmmpKIVnRJKZJYGuI-ON_e21ixX4LxYaKegrmUDZuUEZyTN8pzTQLINqaxxzkIlWqsX0r4LgsW6oFjXEes6IskFE5uCwTv75intP0t5K3X9p403tjbtvxee_FR-RUVbVgE_2r5vbprZMnyJmEr1UukaBKUZK0Jo-gFviaEm
CitedBy_id crossref_primary_10_1088_1009_0630_13_4_11
crossref_primary_10_1088_1009_0630_16_6_07
crossref_primary_10_1016_j_commatsci_2022_111303
crossref_primary_10_7498_aps_63_079401
crossref_primary_10_1088_0741_3335_53_6_065003
Cites_doi 10.1029/2008JA013068
10.1088/0256-307X/26/3/039401
10.1088/0256-307X/22/6/070
10.1029/2004JA010730
10.1088/0256-307X/25/7/063
10.1029/2004JA010628
10.1029/JA094iA07p08895
10.1029/2006JA012178
10.1029/2007GL029915
10.1029/RS016i006p01179
10.1029/2007GL030040
10.1029/91JA01548
10.1029/2004SW000105
10.1088/0256-307X/21/10/037
10.1029/RG010i004p00951
10.5194/angeo-22-2597-2004
10.1088/0256-307X/21/1/039
10.5194/angeo-22-2565-2004
10.1029/2005JA011462
10.1088/0256-307X/25/12/087
10.1126/science.1074956
10.1029/1998GL900071
10.1029/2008JA013580
10.1088/0256-307X/25/1/091
10.1088/0256-307X/25/9/113
10.1029/2002JA009316
10.1088/0256-307X/22/2/070
10.1029/1999JA000241
ContentType Journal Article
DBID 2RA
92L
CQIGP
W94
~WA
AAYXX
CITATION
7TG
KL.
DOI 10.1088/0256-307x/27/5/055204
DatabaseName 维普期刊资源整合服务平台
中文科技期刊数据库-CALIS站点
中文科技期刊数据库-7.0平台
中文科技期刊数据库-自然科学
中文科技期刊数据库- 镜像站点
CrossRef
Meteorological & Geoastrophysical Abstracts
Meteorological & Geoastrophysical Abstracts - Academic
DatabaseTitle CrossRef
Meteorological & Geoastrophysical Abstracts - Academic
Meteorological & Geoastrophysical Abstracts
DatabaseTitleList Meteorological & Geoastrophysical Abstracts - Academic

DeliveryMethod fulltext_linktorsrc
Discipline Physics
DocumentTitleAlternate Propagation Characteristics of Whistler-Mode Chorus during Geomagnetic Activities
EISSN 1741-3540
EndPage 173
ExternalDocumentID 10_1088_0256_307X_27_5_055204
33659456
GroupedDBID 02O
042
1JI
1PV
1WK
29B
2RA
4.4
5B3
5GY
5VR
5VS
5ZH
7.M
7.Q
92L
AAGCD
AAJIO
AAJKP
AALHV
AAPBV
AATNI
ABHWH
ABPTK
ABQJV
ACAFW
ACGFS
ACHIP
AEFHF
AENEX
AFUIB
AFYNE
AHSEE
AKPSB
ALMA_UNASSIGNED_HOLDINGS
ASPBG
ATQHT
AVWKF
AZFZN
BBWZM
CDYEO
CEBXE
CJUJL
CQIGP
CRLBU
CS3
EBS
EDWGO
EJD
EMSAF
EPQRW
EQZZN
FEDTE
HAK
HVGLF
IHE
IJHAN
IOP
IZVLO
JCGBZ
KNG
KOT
LAP
M45
N5L
N9A
NS0
NT-
NT.
P2P
PJBAE
Q02
R4D
RIN
RNS
RO9
ROL
RPA
RW3
S3P
SY9
T37
UCJ
W28
W94
XPP
~02
~WA
02
MGA
UNR
-SA
-S~
AAYXX
ABJNI
ACARI
ADEQX
AERVB
AGQPQ
AOAED
ARNYC
CAJEA
CITATION
Q--
TGP
U1G
U5K
7TG
KL.
ID FETCH-LOGICAL-c456t-d98cd0b6eef77e49e2b353e192d82e0de50908383faae3e46cac3f3b131a642b3
IEDL.DBID IOP
ISSN 0256-307X
IngestDate Fri Jul 11 00:09:17 EDT 2025
Tue Jul 01 01:34:47 EDT 2025
Thu Apr 24 22:52:03 EDT 2025
Tue Nov 10 14:19:51 EST 2020
Mon May 13 14:49:45 EDT 2019
Thu Nov 24 20:27:24 EST 2022
IsPeerReviewed true
IsScholarly true
Issue 5
Language English
LinkModel DirectLink
MergedId FETCHMERGED-LOGICAL-c456t-d98cd0b6eef77e49e2b353e192d82e0de50908383faae3e46cac3f3b131a642b3
Notes P353.8
11-1959/O4
TN011
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
PQID 851467783
PQPubID 23462
PageCount 4
ParticipantIDs iop_primary_10_1088_0256_307X_27_5_055204
chongqing_backfile_33659456
crossref_primary_10_1088_0256_307X_27_5_055204
proquest_miscellaneous_851467783
crossref_citationtrail_10_1088_0256_307X_27_5_055204
ProviderPackageCode CITATION
AAYXX
PublicationCentury 2000
PublicationDate 2010-05-01
PublicationDateYYYYMMDD 2010-05-01
PublicationDate_xml – month: 05
  year: 2010
  text: 2010-05-01
  day: 01
PublicationDecade 2010
PublicationTitle Chinese physics letters
PublicationTitleAlternate Chinese Physics Letters
PublicationYear 2010
Publisher IOP Publishing
Publisher_xml – name: IOP Publishing
References 22
23
24
25
26
Masson A (27) 2004; 22
Xiao F L (13) 2005; 22
29
Lu Q M (9) 2004; 21
Su Z P (17) 2009; 26
Wang D Y (10) 2004; 21
Xiao F L (21) 2008; 25
Gao H N (28) 2008; 25
Zong Q-G (8) 2008; 51
Zheng H N (15) 2008; 25
11
Xiao F L (12) 2005; 22
14
Su Z P (16) 2008; 25
18
19
1
3
4
5
6
7
Parrot M (2) 2004; 22
20
References_xml – volume: 51
  start-page: 1
  issn: 1006-9321
  year: 2008
  ident: 8
  publication-title: Sci. Chin.
– ident: 29
  doi: 10.1029/2008JA013068
– volume: 26
  start-page: 039401
  issn: 0256-307X
  year: 2009
  ident: 17
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/26/3/039401
– volume: 22
  start-page: 1552
  issn: 0256-307X
  year: 2005
  ident: 12
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/22/6/070
– ident: 18
  doi: 10.1029/2004JA010730
– volume: 25
  start-page: 2562
  issn: 0256-307X
  year: 2008
  ident: 28
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/25/7/063
– ident: 11
  doi: 10.1029/2004JA010628
– ident: 20
  doi: 10.1029/JA094iA07p08895
– ident: 19
  doi: 10.1029/2006JA012178
– ident: 7
  doi: 10.1029/2007GL029915
– ident: 22
  doi: 10.1029/RS016i006p01179
– ident: 4
  doi: 10.1029/2007GL030040
– ident: 24
  doi: 10.1029/91JA01548
– ident: 5
  doi: 10.1029/2004SW000105
– volume: 21
  start-page: 1997
  issn: 0256-307X
  year: 2004
  ident: 10
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/21/10/037
– ident: 25
  doi: 10.1029/RG010i004p00951
– volume: 22
  start-page: 2597
  year: 2004
  ident: 2
  publication-title: Ann. Geophys.
  doi: 10.5194/angeo-22-2597-2004
– volume: 21
  start-page: 129
  issn: 0256-307X
  year: 2004
  ident: 9
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/21/1/039
– volume: 22
  start-page: 2565
  year: 2004
  ident: 27
  publication-title: Ann. Geophys.
  doi: 10.5194/angeo-22-2565-2004
– ident: 3
  doi: 10.1029/2005JA011462
– volume: 25
  start-page: 4493
  issn: 0256-307X
  year: 2008
  ident: 16
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/25/12/087
– ident: 6
  doi: 10.1126/science.1074956
– ident: 1
  doi: 10.1029/1998GL900071
– ident: 14
  doi: 10.1029/2008JA013580
– volume: 25
  start-page: 340
  issn: 0256-307X
  year: 2008
  ident: 21
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/25/1/091
– volume: 25
  start-page: 3515
  issn: 0256-307X
  year: 2008
  ident: 15
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/25/9/113
– ident: 26
  doi: 10.1029/2002JA009316
– volume: 22
  start-page: 517
  issn: 0256-307X
  year: 2005
  ident: 13
  publication-title: Chin. Phys. Lett.
  doi: 10.1088/0256-307X/22/2/070
– ident: 23
  doi: 10.1029/1999JA000241
SSID ssj0011811
Score 1.899289
Snippet A recently introduced ray-tracing method is adopted to study the propagation characteristics of whistler-mode chorus during different geomagnetic activities by...
SourceID proquest
crossref
iop
chongqing
SourceType Aggregation Database
Enrichment Source
Index Database
Publisher
StartPage 170
SubjectTerms 传播特性
位置移动
地球轨道
地磁活动
密度模型
等离子体
计算结果
跟踪方法
Title Propagation Characteristics of Whistler-Mode Chorus during Geomagnetic Activities
URI http://iopscience.iop.org/0256-307X/27/5/055204
https://www.proquest.com/docview/851467783
Volume 27
hasFullText 1
inHoldings 1
isFullTextHit
isPrint
link http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwlV1LT9wwEB7BSkhcaEtBbCmVD3DoIUsSx3kcV6g8KhUWCcTeLMeZLNXSZLuPS399Z5zNCgQScIuisaOMHc83sef7AA4tS0nasvBkpqQXJbn1jEyUR2A4xjhLgijh4uRfl_H5bfRzqIZr0CrT_a4ny5W_R5duJ5-DMv8hGR6HLFTtKxU6_k-K_ZxsXVwNVrsGFK2cQl7boq3YoSTvxV6YT-G-rkZ_KUo8iUvr9PBni7OLOKcfYNDW7TQHTca9xTzv2X_PaRzf-jIfYWuJPkW_mS6fYA2rbdhwp0Dt7DNcD6aUQ4_cYImTp1TOoi7FHbMTP-DUYwU1Mqini5loCh3FGdZ_zKjimkjRt06TgpLwHbg9_XFzcu4tNRc8S1Bq7hVZags_jxHLJMEowzCXSiLhwCIN0S-QAAahtlSWxqDEKLbGylLmgQwMpTK53IVOVVe4B8KWobVxkSkTZBHrgGbStyndNDI1mJsu7K-8TzHbjpmJSksZKzKPuxC146Htkq6cVTMetNs2T1PNvtTsSx0mWunGl13orZpNGr6O1xoc0eCsbF-00ZOi7ML3x3av9CnaqaPpa-UtGFNhvZhpwrcRU_bJL-_obh822zMLfvAVOvPpAg8ICs3zb27-_wcf5_ms
linkProvider IOP Publishing
linkToPdf http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV1LT9wwEB7xUCsuLbRFXaDUh_bQQ3aT-JHkiKAL9EG3UlH3ZjnOZCsBybKPS38947wELQhVvUXRjJXMxJ7P8cw3AO-sayVp88zjieSeiFLrGR5Jj8CwQpVEgYhccfLXM3VyLj6N5XgFjrpamHLaLP19uqyJgmsTNglx8cBFaffLZDwIXedqX8rQF4Nplq_CuuQqcYldp99G3VkCxbCqb16r1tbxPDSUY1n4VRaTa4odd6LVKj3RX0t2FYeGzwHbN6jTTy76y0Xat7__IHf831fchGcNUGUHtc4WrGDxAp5UCaN2_hK-j2a03Z5UfmWHd1mfWZmzn47I-BJnnmu2RgLlbDlndU0kO8byykwKVz7JDmzVvoL266_gfPjxx-GJ17Rn8CyhroWXJbHN_FQh5lGEIsEw5ZIjQcYsDtHPkLAIAbyY58YgR6GssTznacADQ7uelG_DWlEW-BqYzUNrVZZIEyTCtQxNuG9juml4bDA1PdjtXELh3V440irNuZIkrnogWidp2zCbuwYbl7o6YY9j7eypnT11GGmpa3v2oN-pTWtqj8cU3pPDOtl7ZTQ5qQcfbss9MiZrvydNE9ud1pgCy-VcExQWjt2P7_zDcG_h6ehoqL-cnn3ehY0208EP9mBtMVviGwJQi3S_mh83S8oJrg
openUrl ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Propagation+Characteristics+of+Whistler-Mode+Chorus+during+Geomagnetic+Activities&rft.jtitle=Chinese+physics+letters&rft.au=Zhou%2C+Qing-Hua&rft.au=He%2C+Yi-Hua&rft.au=He%2C+Zhao-Guo&rft.au=Yang%2C+Chang&rft.date=2010-05-01&rft.issn=0256-307X&rft.volume=27&rft.issue=5&rft.spage=055204&rft.epage=055204&rft_id=info:doi/10.1088%2F0256-307X%2F27%2F5%2F055204&rft.externalDBID=NO_FULL_TEXT
thumbnail_s http://utb.summon.serialssolutions.com/2.0.0/image/custom?url=http%3A%2F%2Fimage.cqvip.com%2Fvip1000%2Fqk%2F84212X%2F84212X.jpg