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Sökning: WFRF:(Lindqvist P. A) > (2005-2009) > Derivation of inner...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003870naa a2200601 4500
001oai:DiVA.org:kth-17865
003SwePub
008100805s2008 | |||||||||||000 ||eng|
009oai:DiVA.org:uu-149308
024a https://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-178652 URI
024a https://doi.org/10.5194/angeo-26-2887-20082 DOI
024a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-1493082 URI
040 a (SwePub)kthd (SwePub)uu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Matsui, H.4 aut
2451 0a Derivation of inner magnetospheric electric field (UNH-IMEF) model using Cluster data set
264 c 2008-09-23
264 1b Copernicus GmbH,c 2008
338 a print2 rdacarrier
500 a QC 20100525
520 a We derive an inner magnetospheric electric field (UNH-IMEF) model at L=2-10 using primarily Cluster electric field data for more than 5 years between February 2001 and October 2006. This electric field data set is divided into several ranges of the interplanetary electric field (IEF) values measured by ACE. As ring current simulations which require electric field as an input parameter are often performed at L=2-6.6, we have included statistical results from ground radars and low altitude satellites inside the perigee of Cluster in our data set (L similar to 4). Electric potential patterns are derived from the average electric fields by solving an inverse problem. The electric potential pattern for small IEF values is probably affected by the ionospheric dynamo. The magnitudes of the electric field increase around the evening local time as IEF increases, presumably due to the sub-auroral polarization stream (SAPS). Another region with enhanced electric fields during large IEF periods is located around 9 MLT at L>8, which is possibly related to solar wind-magnetosphere coupling. Our potential patterns are consistent with those derived from self-consistent simulations. As the potential patterns can be interpolated/extrapolated to any discrete IEF value within measured ranges, we thus derive an empirical electric potential model. The performance of the model is evaluated by comparing the electric field derived from the model with original one measured by Cluster and mapped to the equator. The model is open to the public through our website.
650 7a NATURVETENSKAPx Fysik0 (SwePub)1032 hsv//swe
650 7a NATURAL SCIENCESx Physical Sciences0 (SwePub)1032 hsv//eng
653 a magnetospheric physics
653 a electric fields
653 a magnetosphere-ionosphere
653 a interactions
653 a solar wind-magnetosphere interactions
653 a latitude plasma convection
653 a ring current
653 a large-scale
653 a solar-wind
653 a outer plasmasphere
653 a imf-dependence
653 a saint-santin
653 a ion drifts
653 a edi
653 a potentials
653 a Physics
700a Puhl-Quinn, P. A.4 aut
700a Jordanova, V. K.4 aut
700a Khotyaintsev, Yuriu Uppsala universitet,Institutet för rymdfysik, Uppsalaavdelningen4 aut0 (Swepub:uu)ykh28990
700a Lindqvist, Per-Arneu KTH,Rymd- och plasmafysik4 aut0 (Swepub:kth)u1yukyk9
700a Torbert, R. B.4 aut
710a Uppsala universitetb Institutet för rymdfysik, Uppsalaavdelningen4 org
773t Annales Geophysicaed : Copernicus GmbHg 26:9, s. 2887-2898q 26:9<2887-2898x 0992-7689x 1432-0576
856u https://www.ann-geophys.net/26/2887/2008/angeo-26-2887-2008.pdf
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-17865
8564 8u https://doi.org/10.5194/angeo-26-2887-2008
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-149308

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