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dc.contributor.author Balsley, Ben B.
dc.contributor.author Rey, Augusto
dc.contributor.author Woodman Pollitt, Ronald Francisco
dc.date.accessioned 2018-07-03T11:17:28Z
dc.date.available 2018-07-03T11:17:28Z
dc.date.issued 1976-03-01
dc.identifier.citation Balsley, B., Rey, A., & Woodman, R. F. (1976). On the plasma instability mechanisms responsible for Esq.==$Journal Geophysical Research, 81$==(7), 1391-1396. https://doi.org/10.1029/JA081i007p01391 es_ES
dc.identifier.uri http://hdl.handle.net/20.500.12816/1644
dc.description.abstract Evidence is presented showing that the gradient drift (type 2) irregularities are the most probable scatterers responsible for equatorial sporadic E (Esq) echoes observed on conventional equatorial ionograms and that the two‐stream (type 1) irregularities are not detectable at ionosonde wavelengths (1–10 MHz). es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher American Geophysical Union es_ES
dc.relation.ispartof urn:issn:0148-0227
dc.rights info:eu-repo/semantics/restrictedAccess es_ES
dc.subject Plasma instabilities es_ES
dc.subject Ionosphere es_ES
dc.subject E Region es_ES
dc.title On the plasma instability mechanisms responsible for Esq es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#1.05.01 es_ES
dc.identifier.journal Journal de Geophysical Research es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi https://doi.org/10.1029/JA081i007p01391 es_ES

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