An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside
- Autores
- Richard, M. S.; Cravens, T. E.; Wylie, C.; Webb, D.; Chediak, Q.; Mandt, K.; Waite Jr, J. H.; Rymer, A.; Bertucci, Cesar; Wellbrock, A.; Windsor, A.; Coates, A. J.
- Año de publicación
- 2015
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- onization of neutrals by precipitating electrons and ions is the main source of Titan's nightside ionosphere. This paper has two goals: (1) characterization of the role of electron impact ionization on the nightside ionosphere for different magnetospheric conditions and (2) presentation of empirical ion production rates determined using densities measured by the Cassini Ion and Neutral Mass Spectrometer on the nightside. The ionosphere between 1000 and 1400 km is emphasized. We adopt electron fluxes measured by the Cassini Plasma Spectrometer-Electron Spectrometer and the Magnetospheric Imaging Instrument as classified by Rymer et al. (2009). The current paper follows an earlier paper (Paper I), in which we investigated sources of Titan's dayside ionosphere and demonstrated that the photoionization process is well understood. The current paper (Paper II) demonstrates that modeled and empirical ionization rates on the nightside are in agreement with an electron precipitation source above 1100 km. Ion production rate profiles appropriate for different Saturnian magnetospheric conditions, as outlined by Rymer et al., are constructed for various magnetic field topologies. Empirical production rate profiles are generated for deep nightside flybys of Titan. The results also suggest that at lower altitudes (below 1100 km) another source, such as ion precipitation, is probably needed.
Fil: Richard, M. S.. University of Kansas; Estados Unidos. Benedictine College; Estados Unidos
Fil: Cravens, T. E.. University of Kansas; Estados Unidos
Fil: Wylie, C.. University of Kansas; Estados Unidos
Fil: Webb, D.. University of Kansas; Estados Unidos
Fil: Chediak, Q.. University of Kansas; Estados Unidos
Fil: Mandt, K.. Southwest Research Institute; Estados Unidos
Fil: Waite Jr, J. H.. Southwest Research Institute; Estados Unidos
Fil: Rymer, A.. University Johns Hopkins; 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: Wellbrock, A.. University College London; Reino Unido
Fil: Windsor, A.. Benedictine College. Department of Physics and Astronomy; Estados Unidos
Fil: Coates, A. J.. University College London; Reino Unido - Materia
-
TITAN
ELECTRON PRECIPITATION
IONOSPHERE
MAGNETOSPHERE
IONIZATION - 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:11336/17049
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spelling |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightsideRichard, M. S.Cravens, T. E.Wylie, C.Webb, D.Chediak, Q.Mandt, K.Waite Jr, J. H.Rymer, A.Bertucci, CesarWellbrock, A.Windsor, A.Coates, A. J.TITANELECTRON PRECIPITATIONIONOSPHEREMAGNETOSPHEREIONIZATIONhttps://purl.org/becyt/ford/1.3https://purl.org/becyt/ford/1onization of neutrals by precipitating electrons and ions is the main source of Titan's nightside ionosphere. This paper has two goals: (1) characterization of the role of electron impact ionization on the nightside ionosphere for different magnetospheric conditions and (2) presentation of empirical ion production rates determined using densities measured by the Cassini Ion and Neutral Mass Spectrometer on the nightside. The ionosphere between 1000 and 1400 km is emphasized. We adopt electron fluxes measured by the Cassini Plasma Spectrometer-Electron Spectrometer and the Magnetospheric Imaging Instrument as classified by Rymer et al. (2009). The current paper follows an earlier paper (Paper I), in which we investigated sources of Titan's dayside ionosphere and demonstrated that the photoionization process is well understood. The current paper (Paper II) demonstrates that modeled and empirical ionization rates on the nightside are in agreement with an electron precipitation source above 1100 km. Ion production rate profiles appropriate for different Saturnian magnetospheric conditions, as outlined by Rymer et al., are constructed for various magnetic field topologies. Empirical production rate profiles are generated for deep nightside flybys of Titan. The results also suggest that at lower altitudes (below 1100 km) another source, such as ion precipitation, is probably needed.Fil: Richard, M. S.. University of Kansas; Estados Unidos. Benedictine College; Estados UnidosFil: Cravens, T. E.. University of Kansas; Estados UnidosFil: Wylie, C.. University of Kansas; Estados UnidosFil: Webb, D.. University of Kansas; Estados UnidosFil: Chediak, Q.. University of Kansas; Estados UnidosFil: Mandt, K.. Southwest Research Institute; Estados UnidosFil: Waite Jr, J. H.. Southwest Research Institute; Estados UnidosFil: Rymer, A.. University Johns Hopkins; 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: Wellbrock, A.. University College London; Reino UnidoFil: Windsor, A.. Benedictine College. Department of Physics and Astronomy; Estados UnidosFil: Coates, A. J.. University College London; Reino UnidoAmerican Geophysical Union2015-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/17049Richard, M. S.; Cravens, T. E.; Wylie, C.; Webb, D.; Chediak, Q.; et al.; An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside; American Geophysical Union; Journal Of Geophysical Research; 120; 2; 2-2015; 1281-12980148-0227enginfo:eu-repo/semantics/altIdentifier/doi/10.1002/2014JA020343info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/2014JA020343/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 Técnicas2025-09-29T10:08:33Zoai:ri.conicet.gov.ar:11336/17049instacron: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 10:08:33.813CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside |
title |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside |
spellingShingle |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside Richard, M. S. TITAN ELECTRON PRECIPITATION IONOSPHERE MAGNETOSPHERE IONIZATION |
title_short |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside |
title_full |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside |
title_fullStr |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside |
title_full_unstemmed |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside |
title_sort |
An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside |
dc.creator.none.fl_str_mv |
Richard, M. S. Cravens, T. E. Wylie, C. Webb, D. Chediak, Q. Mandt, K. Waite Jr, J. H. Rymer, A. Bertucci, Cesar Wellbrock, A. Windsor, A. Coates, A. J. |
author |
Richard, M. S. |
author_facet |
Richard, M. S. Cravens, T. E. Wylie, C. Webb, D. Chediak, Q. Mandt, K. Waite Jr, J. H. Rymer, A. Bertucci, Cesar Wellbrock, A. Windsor, A. Coates, A. J. |
author_role |
author |
author2 |
Cravens, T. E. Wylie, C. Webb, D. Chediak, Q. Mandt, K. Waite Jr, J. H. Rymer, A. Bertucci, Cesar Wellbrock, A. Windsor, A. Coates, A. J. |
author2_role |
author author author author author author author author author author author |
dc.subject.none.fl_str_mv |
TITAN ELECTRON PRECIPITATION IONOSPHERE MAGNETOSPHERE IONIZATION |
topic |
TITAN ELECTRON PRECIPITATION IONOSPHERE MAGNETOSPHERE IONIZATION |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.3 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
onization of neutrals by precipitating electrons and ions is the main source of Titan's nightside ionosphere. This paper has two goals: (1) characterization of the role of electron impact ionization on the nightside ionosphere for different magnetospheric conditions and (2) presentation of empirical ion production rates determined using densities measured by the Cassini Ion and Neutral Mass Spectrometer on the nightside. The ionosphere between 1000 and 1400 km is emphasized. We adopt electron fluxes measured by the Cassini Plasma Spectrometer-Electron Spectrometer and the Magnetospheric Imaging Instrument as classified by Rymer et al. (2009). The current paper follows an earlier paper (Paper I), in which we investigated sources of Titan's dayside ionosphere and demonstrated that the photoionization process is well understood. The current paper (Paper II) demonstrates that modeled and empirical ionization rates on the nightside are in agreement with an electron precipitation source above 1100 km. Ion production rate profiles appropriate for different Saturnian magnetospheric conditions, as outlined by Rymer et al., are constructed for various magnetic field topologies. Empirical production rate profiles are generated for deep nightside flybys of Titan. The results also suggest that at lower altitudes (below 1100 km) another source, such as ion precipitation, is probably needed. Fil: Richard, M. S.. University of Kansas; Estados Unidos. Benedictine College; Estados Unidos Fil: Cravens, T. E.. University of Kansas; Estados Unidos Fil: Wylie, C.. University of Kansas; Estados Unidos Fil: Webb, D.. University of Kansas; Estados Unidos Fil: Chediak, Q.. University of Kansas; Estados Unidos Fil: Mandt, K.. Southwest Research Institute; Estados Unidos Fil: Waite Jr, J. H.. Southwest Research Institute; Estados Unidos Fil: Rymer, A.. University Johns Hopkins; 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: Wellbrock, A.. University College London; Reino Unido Fil: Windsor, A.. Benedictine College. Department of Physics and Astronomy; Estados Unidos Fil: Coates, A. J.. University College London; Reino Unido |
description |
onization of neutrals by precipitating electrons and ions is the main source of Titan's nightside ionosphere. This paper has two goals: (1) characterization of the role of electron impact ionization on the nightside ionosphere for different magnetospheric conditions and (2) presentation of empirical ion production rates determined using densities measured by the Cassini Ion and Neutral Mass Spectrometer on the nightside. The ionosphere between 1000 and 1400 km is emphasized. We adopt electron fluxes measured by the Cassini Plasma Spectrometer-Electron Spectrometer and the Magnetospheric Imaging Instrument as classified by Rymer et al. (2009). The current paper follows an earlier paper (Paper I), in which we investigated sources of Titan's dayside ionosphere and demonstrated that the photoionization process is well understood. The current paper (Paper II) demonstrates that modeled and empirical ionization rates on the nightside are in agreement with an electron precipitation source above 1100 km. Ion production rate profiles appropriate for different Saturnian magnetospheric conditions, as outlined by Rymer et al., are constructed for various magnetic field topologies. Empirical production rate profiles are generated for deep nightside flybys of Titan. The results also suggest that at lower altitudes (below 1100 km) another source, such as ion precipitation, is probably needed. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-02 |
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/11336/17049 Richard, M. S.; Cravens, T. E.; Wylie, C.; Webb, D.; Chediak, Q.; et al.; An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside; American Geophysical Union; Journal Of Geophysical Research; 120; 2; 2-2015; 1281-1298 0148-0227 |
url |
http://hdl.handle.net/11336/17049 |
identifier_str_mv |
Richard, M. S.; Cravens, T. E.; Wylie, C.; Webb, D.; Chediak, Q.; et al.; An empirical approach to modeling ion production rates in Titan's ionosphere II: Ion production rates on the nightside; American Geophysical Union; Journal Of Geophysical Research; 120; 2; 2-2015; 1281-1298 0148-0227 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1002/2014JA020343 info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/2014JA020343/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 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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1844613954166325248 |
score |
13.070432 |