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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZGivnK2Y/RNVTS
Repositorysid.inpe.br/mtc-m17@80/2007/10.19.20.42   (restricted access)
Last Update2007:11.27.11.54.47 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m17@80/2007/10.19.20.43.02
Metadata Last Update2021:07.18.04.01.34 (UTC) administrator
Secondary KeyINPE-14987-PRE/9898
ISSN1364-6826
Citation KeyLucasGEGLSVS:2007:EnBaDu
TitleEnergy Balance during Intense and Super-Intense Magnetic Storms using an Akasofu Epsilon Parameter Corrected by The Solar Wind Dynamic Pressure
Year2007
Access Date2024, May 17
Secondary TypePRE PI
Number of Files1
Size757 KiB
2. Context
Author1 Lucas, Aline de
2 Gonzalez, Walter Demé
3 trio
4 Echer, Ezequiel
5 Guarnieri, Luis Fernando
6 Lago, Alisson Dal
7 Silva, Marlos Rockenbach da
8 Vieria, Luis Eduardo Antunes
9 Schuch, Nelson Jorge
Resume Identifier1
2
3
4 8JMKD3MGP5W/3C9JH3D
5
6 8JMKD3MGP5W/3C9JGH3
7
8
9 8JMKD3MGP5W/3C9JHUD
Group1 DGE-INPE-MCT-BR
2 DGE-INPE-MCT-BR
3 DGE-INPE-MCT-BR
4 DGE-INPE-MCT-BR
5 DGE-INPE-MCT-BR
6 DGE-INPE-MCT-BR
7 DGE-INPE-MCT-BR
8 RSU-INPE-MCT-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Instituto Nacional de Pesquisas Espaciais (INPE)
8 Centro Regional Sul de Pesquisas Espaciais (CRS/INPE)
JournalJournal of Atmospheric and Solar-Terrestrial Physics
Volume69
Number15
Pages1851-1863
History (UTC)2007-12-19 14:19:02 :: martaseeger -> administrator ::
2021-07-18 04:01:34 :: administrator -> martaseeger :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsSuper-intense magnetic storms
Energy transfer
å parameter
AbstractGeomagnetic storms are large disturbances in the Earth's magnetosphere caused by enhanced solar windmagnetosphere energy transfer. One of the main manifestations of a geomagnetic storm is the ring current enhancement. It is responsible for the decrease in the geomagnetic field observed at ground stations. In this work, we study the ring current dynamics during two different levels of magnetic storms. Thirty-three events are selected during the period 19812004. Eighteen out of 33 events are very intense (or super-intense) magnetic storms (Dst −250 nT) and the remaining are intense magnetic storms (−250<Dst −100 nT). Interplanetary data from spacecraft in the solar wind near Earth's orbit (ACE, IMP-8, ISEE-3) and geomagnetic indices (Dst and Sym-H) are analyzed. Our aim is to evaluate the interplanetary characteristics (interplanetary dawndusk electric field, interplanetary magnetic field component BS), the å parameter, and the total energy input into the magnetosphere (Wå) for these two classes of magnetic storms. Two corrections on the å energy coupling function are made: the first one is an already known correction in the magnetopause radius to take into account the variation in the solar wind pressure. The second correction on the Akasofu parameter, first proposed in this work, accounts for the reconnection efficiency as a function of the solar wind ram pressure. Geomagnetic data/indices are also employed to study the ring current dynamics and to search for the differences in the storm evolution during these events. Our corrected å parameter is shown to be more adequate to explain storm energy balance because the energy input and the energy dissipated in the ring current are in better agreement with modern estimates as compared with previous works. For super-intense storms, the correction of the Akasofu å is on average a scaling factor of 3.7, whilst for intense events, this scaling factor is on average 3.4. The injected energy during the main phase using corrected å can be considered a criterion to separate intense from very intense storms. Other possibilities of cutoff values based on the energy input are also investigated. A threshold value for the input energy is much more clear when a new classification on Dst=−165 nT is considered. It was found that the energy input during storms with Dst<−165 nT is double of the energy for storms with Dst>−165 nT.
AreaCEA
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4. Conditions of access and use
Languageen
Target FileEnergy balance during.pdf
User Groupadministrator
martaseeger
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/3EUFCFP
DisseminationWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Host Collectionlcp.inpe.br/ignes/2004/02.12.18.39
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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7. Description control
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