Pseudobreakups dring January 10, 1997

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dc.contributor.author Arballo, J.K.
dc.contributor.author Ho, Christian M.
dc.contributor.author Lakhina, G.S.
dc.contributor.author Tsurutani, B.T.
dc.contributor.author Zhou, X.-Y.
dc.contributor.author Kamide, Y.
dc.contributor.author Shue, J.-H.
dc.contributor.author Akasofu, S.-I.
dc.contributor.author Lepping, R.P.
dc.contributor.author Goodrich, C.C.
dc.contributor.author Papadopoulos, K.
dc.contributor.author Sharma, A.S.
dc.contributor.author Lyon, J.G.
dc.date.accessioned 2015-09-29T06:15:38Z
dc.date.accessioned 2021-02-12T09:30:13Z
dc.date.available 2015-09-29T06:15:38Z
dc.date.available 2021-02-12T09:30:13Z
dc.date.issued 1998
dc.identifier.citation SUBSTORMS-4, edited by S.Kokuburn and Y.Kamide, p.315-318, 1998 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/502
dc.description.abstract The January 10, 1997 interplanetary pressure pulse (observed at 0053 UT at Wind) caused a dayside aurora, as seen in Polar Ultraviolet Imager (UVI) data that propagates tailward and to lower L. After the solar wind has propagated -150 Re, downtail, a substorm pseu-dobreakup (PB) was detected at 68" N magnetic latitude, at local midnight. The PB dimmed on time scales of minutes and rebrightened 9 min. later. This happened several times in succession. A quasiperiod of approximately 10 min. was noted. The scale size of the PBs was -200 by 200 km in the ionosphere and there was no evidence of eastward drifts of the electrons causing the aurorat brightening. en_US
dc.language.iso en en_US
dc.subject Pseudobreakups en_US
dc.subject Ultraviolet imager en_US
dc.subject Solar wind en_US
dc.subject UVI images en_US
dc.title Pseudobreakups dring January 10, 1997 en_US
dc.type Article en_US
dc.identifier.accession 091013


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