dc.creatorShume, E. B.
dc.creatorDe Paula, E. R.
dc.creatorMaus, S.
dc.creatorHysell, D. L.
dc.creatorRodrigues, F. S.
dc.creatorBekele, A.
dc.date.accessioned2018-11-05T14:50:01Z
dc.date.accessioned2023-05-24T14:22:35Z
dc.date.available2018-11-05T14:50:01Z
dc.date.available2023-05-24T14:22:35Z
dc.date.created2018-11-05T14:50:01Z
dc.date.issued2009-06-06
dc.identifierShume, E. B., De Paula, E. R., Maus, S., Hysell, D. L., Rodrigues, F. S., & Bekele, A. (2009). Equatorial zonal electric fields inferred from a 3‐D electrostatic potential model and ground‐based magnetic field measurements.==$Journal of Geophysical Research: Space Physics, 114$==(A6), A06305. https://doi.org/10.1029/2009JA014158
dc.identifierhttp://hdl.handle.net/20.500.12816/3282
dc.identifierJournal of Geophysical Research: Space Physics
dc.identifierhttps://doi.org/10.1029/2009JA014158
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/6428973
dc.description.abstractWe present a new technique to infer quiet time zonal electric fields in the daytime equatorial ionosphere. The electric field inference technique utilizes a three‐dimensional (3‐D) electrostatic potential model of the low‐latitude ionosphere constrained by ground‐based magnetic field measurements. To test this technique, inferred zonal electric fields for the Peruvian sector in Jicamarca (11.95°S, 283.13°E, 0.6°N dip latitude) were compared with zonal electric field (vertical drift) measurements made by the Jicamarca Incoherent Scatter Radar. The comparison shows a good agreement between the inferred and measured electric fields. An example of electric field estimation for Davao (7.4°N, 125.4°E, 0.58°S dip latitude) in the Philippines sector is also presented in this report. Inferred electric fields for Davao are in good agreement with F region vertical plasma drifts measured by drift sensors onboard the AE‐E and ROCSAT‐1 satellites on that longitude sector. Our results suggest that realistic estimates of quiet time zonal electric fields for the equatorial ionosphere can be obtained from the 3‐D potential model whenever observatory magnetic field measurements are available.
dc.languageeng
dc.publisherAmerican Geophysical Union
dc.relationurn:issn:2169-9380
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectElectric zonal fields
dc.subjectRadar
dc.subjectMagnetic fields
dc.titleEquatorial zonal electric fields inferred from a 3‐D electrostatic potential model and ground‐based magnetic field measurements
dc.typeinfo:eu-repo/semantics/article


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