Westward ionospheric electric field perturbations on the dayside associated with substorm processes

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dc.contributor.author Wei, Y.
dc.contributor.author Pu, Z.
dc.contributor.author Hong, M.
dc.contributor.author Zong, Q.
dc.contributor.author Ren, Z.
dc.contributor.author Fu, S.
dc.contributor.author Xie, L.
dc.contributor.author Alex, S.
dc.contributor.author Cao, X.
dc.contributor.author Wang, J.
dc.contributor.author Chu, X.
dc.date.accessioned 2015-10-08T05:16:57Z
dc.date.accessioned 2021-02-12T09:21:07Z
dc.date.available 2015-10-08T05:16:57Z
dc.date.available 2021-02-12T09:21:07Z
dc.date.issued 2009
dc.identifier.citation JGR, v.114, A12209, 2009, doi: 10.1029/2009JA014445 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/561
dc.description.abstract [1] A controversy has risen in the direction of ionospheric electric field perturbation on the dayside caused by substorm expansion phase in recent years, i.e., eastward or westward. To exclude the effect of interplanetary magnetic field northward turning, the substorms without interplanetary field (IMF) trigger are required to investigate this issue. Previous works, such as that by Huang et al. (2004), showed that the eastward electric field perturbations caused by substorms can be observed. However, our case suggests that some substorms can produce strong westward electric field perturbations and drive westward equatorial electrojets on the dayside ionosphere. This westward electric field is created by an overshielding-like imbalance state of field-aligned currents (FACs), Region 2 (R2) FAC greater than Region 1 (R1) FAC, which is built up through R2 FAC enhancement rather than R1 FAC reduction due to IMF northward turning. The substorm processes should be responsible for the westward electric field especially through polar cap shrinkage and magnetic field dipolarization. en_US
dc.language.iso en en_US
dc.subject Ionospheric electric field en_US
dc.subject Interplanetary magnetic field en_US
dc.subject Field-aligned currents en_US
dc.title Westward ionospheric electric field perturbations on the dayside associated with substorm processes en_US
dc.type Article en_US
dc.identifier.accession 091080


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