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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/20436
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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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1844613147428651008 |
score |
13.070432 |