Observations of E region field-aligned irregularities just outside the equatorial electrojet region

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We have used the Piura VHF radar (5° 12’S, 80°38’W, ~7.5°N dip latitude), just outside the equatorial electrojet region, in northern Perú (see Figure 1) to gather echoes from 3-m E region field-aligned irregularities (FAI). Our observations are based on short campaigns of few consecutive days taken...

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Detalles Bibliográficos
Autores: Chau Chong Shing, Jorge Luis, Woodman Pollitt, Ronald Francisco, Flores, L.A.
Formato: documento de trabajo
Fecha de Publicación:2000
Institución:Instituto Geofísico del Perú
Repositorio:IGP-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.igp.gob.pe:20.500.12816/523
Enlace del recurso:http://hdl.handle.net/20.500.12816/523
Nivel de acceso:acceso abierto
Materia:E Region
Equatorial Electrojet
Echoes
Radar
http://purl.org/pe-repo/ocde/ford#1.05.01
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dc.title.none.fl_str_mv Observations of E region field-aligned irregularities just outside the equatorial electrojet region
title Observations of E region field-aligned irregularities just outside the equatorial electrojet region
spellingShingle Observations of E region field-aligned irregularities just outside the equatorial electrojet region
Chau Chong Shing, Jorge Luis
E Region
Equatorial Electrojet
Echoes
Radar
http://purl.org/pe-repo/ocde/ford#1.05.01
title_short Observations of E region field-aligned irregularities just outside the equatorial electrojet region
title_full Observations of E region field-aligned irregularities just outside the equatorial electrojet region
title_fullStr Observations of E region field-aligned irregularities just outside the equatorial electrojet region
title_full_unstemmed Observations of E region field-aligned irregularities just outside the equatorial electrojet region
title_sort Observations of E region field-aligned irregularities just outside the equatorial electrojet region
author Chau Chong Shing, Jorge Luis
author_facet Chau Chong Shing, Jorge Luis
Woodman Pollitt, Ronald Francisco
Flores, L.A.
author_role author
author2 Woodman Pollitt, Ronald Francisco
Flores, L.A.
author2_role author
author
dc.contributor.author.fl_str_mv Chau Chong Shing, Jorge Luis
Woodman Pollitt, Ronald Francisco
Flores, L.A.
dc.subject.none.fl_str_mv E Region
Equatorial Electrojet
Echoes
Radar
topic E Region
Equatorial Electrojet
Echoes
Radar
http://purl.org/pe-repo/ocde/ford#1.05.01
dc.subject.ocde.none.fl_str_mv http://purl.org/pe-repo/ocde/ford#1.05.01
description We have used the Piura VHF radar (5° 12’S, 80°38’W, ~7.5°N dip latitude), just outside the equatorial electrojet region, in northern Perú (see Figure 1) to gather echoes from 3-m E region field-aligned irregularities (FAI). Our observations are based on short campaigns of few consecutive days taken since 1995 at different times of the year. E region FAIs over Piura are confined to the 95-120 km altitude and present spectral characteristics similar to type 2 equatorial electrojet (EEJ) echoes. However, despite of being at only 7°N dip latitude, they appear mainly at nighttime and early morning, and thus do not present a temporal similarity to the EEJ. We observe the existence of two well-defined types of echoes: 1) lower E region echoes (95-105 km), and upper E region echoes (105-120 km). The lower echoes present a layering characteristic while the upper layer is more structured. In this latter region, the so-called quasiperiodic (QP) echoes have been observed with positive, vertical, and negative slopes and their characteristics are compared to those observed at mid latitudes. In addition, a relationship between concurrent E region irregularities over Piura and F region irregularities over Piura and Jicamarca is presented.
publishDate 2000
dc.date.accessioned.none.fl_str_mv 2016-11-08T05:53:05Z
2017-12-21T19:41:40Z
dc.date.available.none.fl_str_mv 2016-11-08T05:53:05Z
2017-12-21T19:41:40Z
dc.date.issued.fl_str_mv 2000
dc.type.none.fl_str_mv info:eu-repo/semantics/workingPaper
format workingPaper
dc.identifier.citation.none.fl_str_mv Chau, J. L, Woodman, R. F., & Flores, L. A. (2000). Observations of E region field-aligned irregularities just outside the equatorial electrojet region.
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/20.500.12816/523
identifier_str_mv Chau, J. L, Woodman, R. F., & Flores, L. A. (2000). Observations of E region field-aligned irregularities just outside the equatorial electrojet region.
url http://hdl.handle.net/20.500.12816/523
dc.language.iso.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.uri.none.fl_str_mv https://creativecommons.org/licences/by/4.0/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licences/by/4.0/
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Instituto Geofísico del Perú, Radio Observatorio de Jicamarca
publisher.none.fl_str_mv Instituto Geofísico del Perú, Radio Observatorio de Jicamarca
dc.source.none.fl_str_mv reponame:IGP-Institucional
instname:Instituto Geofísico del Perú
instacron:IGP
instname_str Instituto Geofísico del Perú
instacron_str IGP
institution IGP
reponame_str IGP-Institucional
collection IGP-Institucional
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spelling Chau Chong Shing, Jorge LuisWoodman Pollitt, Ronald FranciscoFlores, L.A.2016-11-08T05:53:05Z2017-12-21T19:41:40Z2016-11-08T05:53:05Z2017-12-21T19:41:40Z2000Chau, J. L, Woodman, R. F., & Flores, L. A. (2000). Observations of E region field-aligned irregularities just outside the equatorial electrojet region.http://hdl.handle.net/20.500.12816/523We have used the Piura VHF radar (5° 12’S, 80°38’W, ~7.5°N dip latitude), just outside the equatorial electrojet region, in northern Perú (see Figure 1) to gather echoes from 3-m E region field-aligned irregularities (FAI). Our observations are based on short campaigns of few consecutive days taken since 1995 at different times of the year. E region FAIs over Piura are confined to the 95-120 km altitude and present spectral characteristics similar to type 2 equatorial electrojet (EEJ) echoes. However, despite of being at only 7°N dip latitude, they appear mainly at nighttime and early morning, and thus do not present a temporal similarity to the EEJ. We observe the existence of two well-defined types of echoes: 1) lower E region echoes (95-105 km), and upper E region echoes (105-120 km). The lower echoes present a layering characteristic while the upper layer is more structured. In this latter region, the so-called quasiperiodic (QP) echoes have been observed with positive, vertical, and negative slopes and their characteristics are compared to those observed at mid latitudes. 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