Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus

Autores
Cravens, T. E.; Richard, M.; Ma, Y. J.; Bertucci, Cesar; Luhmann, J. G.; Ledvina, S.; Robertson, I. P.; Wahlund, J. E.; Ågren, K.; Cui, J.; Muller Wodarg, I.; Waite, J. H.; Dougherty, M.; Bell, J.; Ulusen, D.
Año de publicación
2010
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Plasma in Titan´s ionosphere flows in response to forcing from thermal pressure gradients, magnetic forces, gravity, and ion-neutral collisions. This paper takes an empirical approach to the ionospheric dynamics by using data from Cassini instruments to estimate pressures, flow speeds, and time constants on the dayside and nightside. The plasma flow speed relative to the neutral gas speed is approximately 1 m s‑1 near an altitude of 1000 km and 200 m s‑1 at 1500 km. For comparison, the thermospheric neutral wind speed is about 100 m s‑1. The ionospheric plasma is strongly coupled to the neutrals below an altitude of about 1300 km. Transport, vertical or horizontal, becomes more important than chemistry in controlling ionospheric densities above about 1200-1500 km, depending on the ion species. Empirical estimates are used to demonstrate that the structure of the ionospheric magnetic field is determined by plasma transport (including neutral wind effects) for altitudes above about 1000 km and by magnetic diffusion at lower altitudes. The paper suggests that a velocity shear layer near 1300 km could exist at some locations and could affect the structure of the magnetic field. Both Hall and polarization electric field terms in the magnetic induction equation are shown to be locally important in controlling the structure of Titan´s ionospheric magnetic field. Comparisons are made between the ionospheric dynamics at Titan and at Venus.
Fil: Cravens, T. E.. University of Kansas; Estados Unidos
Fil: Richard, M.. University of Kansas; Estados Unidos
Fil: Ma, Y. J.. University of California; Estados Unidos
Fil: Bertucci, Cesar. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina
Fil: Luhmann, J. G.. University of California; Estados Unidos
Fil: Ledvina, S.. University of California; Estados Unidos
Fil: Robertson, I. P.. University of Kansas; Estados Unidos
Fil: Wahlund, J. E.. Swedish Institute of Space Physics; Suecia
Fil: Ågren, K.. Swedish Institute of Space Physics; Suecia
Fil: Cui, J.. Imperial College London; Reino Unido
Fil: Muller Wodarg, I.. Imperial College London; Reino Unido
Fil: Waite, J. H.. Southwest Research Institute; Estados Unidos
Fil: Dougherty, M.. Imperial College London; Reino Unido
Fil: Bell, J.. Southwest Research Institute; Estados Unidos
Fil: Ulusen, D.. University of California; Estados Unidos
Materia
Ionosphere: Ionosphere/magnetosphere interactions
Ionosphere: Ionosphere/atmosphere interactions
Ionosphere: Ionospheric dynamics
Planetary Sciences: Comets and Small Bodies: Ionospheres (2459), Planetary Sciences: Solar System Objects: Titan
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/20436

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network_name_str CONICET Digital (CONICET)
spelling Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with VenusCravens, T. E.Richard, M.Ma, Y. J.Bertucci, CesarLuhmann, J. G.Ledvina, S.Robertson, I. P.Wahlund, J. E.Ågren, K.Cui, J.Muller Wodarg, I.Waite, J. H.Dougherty, M.Bell, J.Ulusen, D.Ionosphere: Ionosphere/magnetosphere interactionsIonosphere: Ionosphere/atmosphere interactionsIonosphere: Ionospheric dynamicsPlanetary Sciences: Comets and Small Bodies: Ionospheres (2459), Planetary Sciences: Solar System Objects: Titanhttps://purl.org/becyt/ford/1.3https://purl.org/becyt/ford/1Plasma in Titan´s ionosphere flows in response to forcing from thermal pressure gradients, magnetic forces, gravity, and ion-neutral collisions. This paper takes an empirical approach to the ionospheric dynamics by using data from Cassini instruments to estimate pressures, flow speeds, and time constants on the dayside and nightside. The plasma flow speed relative to the neutral gas speed is approximately 1 m s<sup>‑1</sup> near an altitude of 1000 km and 200 m s<sup>‑1</sup> at 1500 km. For comparison, the thermospheric neutral wind speed is about 100 m s<sup>‑1</sup>. The ionospheric plasma is strongly coupled to the neutrals below an altitude of about 1300 km. Transport, vertical or horizontal, becomes more important than chemistry in controlling ionospheric densities above about 1200-1500 km, depending on the ion species. Empirical estimates are used to demonstrate that the structure of the ionospheric magnetic field is determined by plasma transport (including neutral wind effects) for altitudes above about 1000 km and by magnetic diffusion at lower altitudes. The paper suggests that a velocity shear layer near 1300 km could exist at some locations and could affect the structure of the magnetic field. Both Hall and polarization electric field terms in the magnetic induction equation are shown to be locally important in controlling the structure of Titan´s ionospheric magnetic field. Comparisons are made between the ionospheric dynamics at Titan and at Venus.Fil: Cravens, T. E.. University of Kansas; Estados UnidosFil: Richard, M.. University of Kansas; Estados UnidosFil: Ma, Y. J.. University of California; Estados UnidosFil: Bertucci, Cesar. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; ArgentinaFil: Luhmann, J. G.. University of California; Estados UnidosFil: Ledvina, S.. University of California; Estados UnidosFil: Robertson, I. P.. University of Kansas; Estados UnidosFil: Wahlund, J. E.. Swedish Institute of Space Physics; SueciaFil: Ågren, K.. Swedish Institute of Space Physics; SueciaFil: Cui, J.. Imperial College London; Reino UnidoFil: Muller Wodarg, I.. Imperial College London; Reino UnidoFil: Waite, J. H.. Southwest Research Institute; Estados UnidosFil: Dougherty, M.. Imperial College London; Reino UnidoFil: Bell, J.. Southwest Research Institute; Estados UnidosFil: Ulusen, D.. University of California; Estados UnidosAmerican Geophysical Union2010-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/20436Cravens, T. E.; Richard, M.; Ma, Y. J.; Bertucci, Cesar; Luhmann, J. G.; et al.; Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus; American Geophysical Union; Journal of Geophysical Research; 115; A08319; 10-2010; 1-170148-0227CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1029/2009JA015050info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1029/2009JA015050/abstractinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:36:34Zoai:ri.conicet.gov.ar:11336/20436instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:36:34.256CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
title Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
spellingShingle Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
Cravens, T. E.
Ionosphere: Ionosphere/magnetosphere interactions
Ionosphere: Ionosphere/atmosphere interactions
Ionosphere: Ionospheric dynamics
Planetary Sciences: Comets and Small Bodies: Ionospheres (2459), Planetary Sciences: Solar System Objects: Titan
title_short Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
title_full Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
title_fullStr Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
title_full_unstemmed Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
title_sort Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus
dc.creator.none.fl_str_mv Cravens, T. E.
Richard, M.
Ma, Y. J.
Bertucci, Cesar
Luhmann, J. G.
Ledvina, S.
Robertson, I. P.
Wahlund, J. E.
Ågren, K.
Cui, J.
Muller Wodarg, I.
Waite, J. H.
Dougherty, M.
Bell, J.
Ulusen, D.
author Cravens, T. E.
author_facet Cravens, T. E.
Richard, M.
Ma, Y. J.
Bertucci, Cesar
Luhmann, J. G.
Ledvina, S.
Robertson, I. P.
Wahlund, J. E.
Ågren, K.
Cui, J.
Muller Wodarg, I.
Waite, J. H.
Dougherty, M.
Bell, J.
Ulusen, D.
author_role author
author2 Richard, M.
Ma, Y. J.
Bertucci, Cesar
Luhmann, J. G.
Ledvina, S.
Robertson, I. P.
Wahlund, J. E.
Ågren, K.
Cui, J.
Muller Wodarg, I.
Waite, J. H.
Dougherty, M.
Bell, J.
Ulusen, D.
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Ionosphere: Ionosphere/magnetosphere interactions
Ionosphere: Ionosphere/atmosphere interactions
Ionosphere: Ionospheric dynamics
Planetary Sciences: Comets and Small Bodies: Ionospheres (2459), Planetary Sciences: Solar System Objects: Titan
topic Ionosphere: Ionosphere/magnetosphere interactions
Ionosphere: Ionosphere/atmosphere interactions
Ionosphere: Ionospheric dynamics
Planetary Sciences: Comets and Small Bodies: Ionospheres (2459), Planetary Sciences: Solar System Objects: Titan
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Plasma in Titan´s ionosphere flows in response to forcing from thermal pressure gradients, magnetic forces, gravity, and ion-neutral collisions. This paper takes an empirical approach to the ionospheric dynamics by using data from Cassini instruments to estimate pressures, flow speeds, and time constants on the dayside and nightside. The plasma flow speed relative to the neutral gas speed is approximately 1 m s<sup>‑1</sup> near an altitude of 1000 km and 200 m s<sup>‑1</sup> at 1500 km. For comparison, the thermospheric neutral wind speed is about 100 m s<sup>‑1</sup>. The ionospheric plasma is strongly coupled to the neutrals below an altitude of about 1300 km. Transport, vertical or horizontal, becomes more important than chemistry in controlling ionospheric densities above about 1200-1500 km, depending on the ion species. Empirical estimates are used to demonstrate that the structure of the ionospheric magnetic field is determined by plasma transport (including neutral wind effects) for altitudes above about 1000 km and by magnetic diffusion at lower altitudes. The paper suggests that a velocity shear layer near 1300 km could exist at some locations and could affect the structure of the magnetic field. Both Hall and polarization electric field terms in the magnetic induction equation are shown to be locally important in controlling the structure of Titan´s ionospheric magnetic field. Comparisons are made between the ionospheric dynamics at Titan and at Venus.
Fil: Cravens, T. E.. University of Kansas; Estados Unidos
Fil: Richard, M.. University of Kansas; Estados Unidos
Fil: Ma, Y. J.. University of California; Estados Unidos
Fil: Bertucci, Cesar. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina
Fil: Luhmann, J. G.. University of California; Estados Unidos
Fil: Ledvina, S.. University of California; Estados Unidos
Fil: Robertson, I. P.. University of Kansas; Estados Unidos
Fil: Wahlund, J. E.. Swedish Institute of Space Physics; Suecia
Fil: Ågren, K.. Swedish Institute of Space Physics; Suecia
Fil: Cui, J.. Imperial College London; Reino Unido
Fil: Muller Wodarg, I.. Imperial College London; Reino Unido
Fil: Waite, J. H.. Southwest Research Institute; Estados Unidos
Fil: Dougherty, M.. Imperial College London; Reino Unido
Fil: Bell, J.. Southwest Research Institute; Estados Unidos
Fil: Ulusen, D.. University of California; Estados Unidos
description Plasma in Titan´s ionosphere flows in response to forcing from thermal pressure gradients, magnetic forces, gravity, and ion-neutral collisions. This paper takes an empirical approach to the ionospheric dynamics by using data from Cassini instruments to estimate pressures, flow speeds, and time constants on the dayside and nightside. The plasma flow speed relative to the neutral gas speed is approximately 1 m s<sup>‑1</sup> near an altitude of 1000 km and 200 m s<sup>‑1</sup> at 1500 km. For comparison, the thermospheric neutral wind speed is about 100 m s<sup>‑1</sup>. The ionospheric plasma is strongly coupled to the neutrals below an altitude of about 1300 km. Transport, vertical or horizontal, becomes more important than chemistry in controlling ionospheric densities above about 1200-1500 km, depending on the ion species. Empirical estimates are used to demonstrate that the structure of the ionospheric magnetic field is determined by plasma transport (including neutral wind effects) for altitudes above about 1000 km and by magnetic diffusion at lower altitudes. The paper suggests that a velocity shear layer near 1300 km could exist at some locations and could affect the structure of the magnetic field. Both Hall and polarization electric field terms in the magnetic induction equation are shown to be locally important in controlling the structure of Titan´s ionospheric magnetic field. Comparisons are made between the ionospheric dynamics at Titan and at Venus.
publishDate 2010
dc.date.none.fl_str_mv 2010-10
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/20436
Cravens, T. E.; Richard, M.; Ma, Y. J.; Bertucci, Cesar; Luhmann, J. G.; et al.; Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus; American Geophysical Union; Journal of Geophysical Research; 115; A08319; 10-2010; 1-17
0148-0227
CONICET Digital
CONICET
url http://hdl.handle.net/11336/20436
identifier_str_mv Cravens, T. E.; Richard, M.; Ma, Y. J.; Bertucci, Cesar; Luhmann, J. G.; et al.; Dynamical and magnetic field time constants for Titan's ionosphere: Empirical estimates and comparisons with Venus; American Geophysical Union; Journal of Geophysical Research; 115; A08319; 10-2010; 1-17
0148-0227
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1029/2009JA015050
info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1029/2009JA015050/abstract
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv American Geophysical Union
publisher.none.fl_str_mv American Geophysical Union
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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