Global expansion of the dayside magnetopause for long-duration radial IMF events: Statistical study on GOES observations
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F16%3A10334297" target="_blank" >RIV/00216208:11320/16:10334297 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1002/2016JA022772" target="_blank" >http://dx.doi.org/10.1002/2016JA022772</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1002/2016JA022772" target="_blank" >10.1002/2016JA022772</a>
Alternative languages
Result language
angličtina
Original language name
Global expansion of the dayside magnetopause for long-duration radial IMF events: Statistical study on GOES observations
Original language description
For decades, unusual locations of the magnetopause under radial interplanetary magnetic field (IMF) have been reported in many studies using in situ satellite observations. These studies have shown that the magnetopause is expanded either over all magnetic local times (MLTs) on the dayside (global expansion) or just near the noon (bullet-like expansion) during radial IMF conditions. With limited observations near the magnetopause, the type of the magnetopause expansion is still undetermined. In this study, 19years of dayside geosynchronous magnetic field data obtained from Geostationary Operational Environmental Satellites (GOES) are statistically processed to infer the shape of the dayside magnetopause under radial IMF conditions. The MLT distributions of geosynchronous magnetic fields for radial IMF are compared with those for northward IMF with the correction of solar wind dynamic pressure distributions between two different IMF conditions. After removal of the solar wind dynamic pressure effect, we have found that the geosynchronous magnetic field for radial IMF is smaller than that for northward IMF over almost all MLTs on the dayside regardless of magnetic latitudes and seasons. The difference between geosynchronous magnetic fields for the northward and radial IMFs supports the suggestion that the dayside magnetopause is globally expanded during the radial IMF conditions.
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
BL - Plasma physics and discharge through gases
OECD FORD branch
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Result continuities
Project
<a href="/en/project/GA14-19376S" target="_blank" >GA14-19376S: Driving of the Earth magnetosphere by ICMEs and CIRs</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Geophysical Research - Space Physics
ISSN
2169-9380
e-ISSN
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Volume of the periodical
121
Issue of the periodical within the volume
7
Country of publishing house
US - UNITED STATES
Number of pages
13
Pages from-to
6480-6492
UT code for WoS article
000383422100031
EID of the result in the Scopus database
2-s2.0-84978870789