Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers

Descripción del Articulo

Póster presentado en ISEA12, Greta, Grecia, Mayo 18-25, 2008.
Detalles Bibliográficos
Autores: Pinedo, H., Chau Chong Shing, Jorge Luis, Hysell, D.
Formato: objeto de conferencia
Fecha de Publicación:2008
Institución:Instituto Geofísico del Perú
Repositorio:IGP-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.igp.gob.pe:20.500.12816/3820
Enlace del recurso:http://hdl.handle.net/20.500.12816/3820
Nivel de acceso:acceso abierto
Materia:Radar
Atmosphere
Plasma
http://purl.org/pe-repo/ocde/ford#1.05.01
http://purl.org/pe-repo/ocde/ford#1.05.00
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spelling Pinedo, H.Chau Chong Shing, Jorge LuisHysell, D.2018-11-23T11:21:21Z2018-11-23T11:21:21Z2008http://hdl.handle.net/20.500.12816/3820Póster presentado en ISEA12, Greta, Grecia, Mayo 18-25, 2008.Recently Hysell et al. [2005] has suggested that the periodic structuring observed in the bottomtype (BT) scattering layers might be used to determine the occurrence or not of full-blown equatorial spread F (ESF) on a given day. The seed or precursor waves may be generated by a collisional shear instability. Preliminary observations at Jicamarca and AL TAIR have shown that such structures present wavelengths of the order of tens or hundreds of kilometers. At Jicamarca periodic structures have been observed using in-beam radar imaging techniques, however such observations are limited to few days in the last five years. On the other hand, routine observations using the JULIA system at Jicamarca have been done since 1996 on approximately 100 days per year on average, using interferometric and dual-beam observations with very narrow beams. Since the bottom-type irregularities drift ata relatively constant speed in the westward direction, using the JULIA narrow beams (~1o), the spatial periodicities might be observed as temporal periodicities in typical range-time intensity maps. In this initial work we present the statistics of the observed bottom-type periodicities and the occurrence of ESF plumes as detected with the JULIA system for years 2006-2008. Besides we presenta time occurrence statistics of a weak bottom-type layer that took place previously to bottom-type layers.application/pdfengInstituto Geofísico del Perúinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licences/by/4.0/RadarAtmospherePlasmahttp://purl.org/pe-repo/ocde/ford#1.05.01http://purl.org/pe-repo/ocde/ford#1.05.00Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layersinfo:eu-repo/semantics/conferenceObjectreponame:IGP-Institucionalinstname:Instituto Geofísico del Perúinstacron:IGPORIGINALpinedo2008.pdfpinedo2008.pdfapplication/pdf3570658https://repositorio.igp.gob.pe/bitstreams/e0fc533e-84ae-44a2-b99d-95aea071fb32/downloadfb4ae21e817b3f282db26c25d8c93f84MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-8393https://repositorio.igp.gob.pe/bitstreams/ec35789a-130b-48a0-b335-f97a0c94890d/downloadf6e2e38ecabbf5c802f4b273da8f9399MD52THUMBNAILpinedo2008.pdf.jpgpinedo2008.pdf.jpgIM Thumbnailimage/jpeg103692https://repositorio.igp.gob.pe/bitstreams/e65efd47-20e2-45ef-ade3-fc1bf7c76cac/downloadc051e07a10ed6a14d69773c40d2cc2e9MD53TEXTpinedo2008.pdf.txtpinedo2008.pdf.txtExtracted texttext/plain1https://repositorio.igp.gob.pe/bitstreams/0391560f-5059-4888-a9bc-a85e4969d5bb/download68b329da9893e34099c7d8ad5cb9c940MD5420.500.12816/3820oai:repositorio.igp.gob.pe:20.500.12816/38202021-03-10 12:01:46.584https://creativecommons.org/licences/by/4.0/info:eu-repo/semantics/openAccessopen.accesshttps://repositorio.igp.gob.peRepositorio Geofísico del Perudspace-help@myu.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
dc.title.es_ES.fl_str_mv Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
title Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
spellingShingle Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
Pinedo, H.
Radar
Atmosphere
Plasma
http://purl.org/pe-repo/ocde/ford#1.05.01
http://purl.org/pe-repo/ocde/ford#1.05.00
title_short Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
title_full Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
title_fullStr Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
title_full_unstemmed Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
title_sort Using JULIA long dataset to find preconditioning evidence of ESF in bottom-type layers
author Pinedo, H.
author_facet Pinedo, H.
Chau Chong Shing, Jorge Luis
Hysell, D.
author_role author
author2 Chau Chong Shing, Jorge Luis
Hysell, D.
author2_role author
author
dc.contributor.author.fl_str_mv Pinedo, H.
Chau Chong Shing, Jorge Luis
Hysell, D.
dc.subject.es_ES.fl_str_mv Radar
Atmosphere
Plasma
topic Radar
Atmosphere
Plasma
http://purl.org/pe-repo/ocde/ford#1.05.01
http://purl.org/pe-repo/ocde/ford#1.05.00
dc.subject.ocde.es_ES.fl_str_mv http://purl.org/pe-repo/ocde/ford#1.05.01
http://purl.org/pe-repo/ocde/ford#1.05.00
description Póster presentado en ISEA12, Greta, Grecia, Mayo 18-25, 2008.
publishDate 2008
dc.date.accessioned.none.fl_str_mv 2018-11-23T11:21:21Z
dc.date.available.none.fl_str_mv 2018-11-23T11:21:21Z
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