Long-term geospace climate monitoring

Autores
Zhang, Shun-Rong; Cnossen, Ingrid; Laštovička, Jan; Elias, Ana Georgina; Yue, Xinan; Jacobi, Christoph; Yue, Jia; Wang, Wenbin; Qian, Liying; Goncharenko, Larisa
Año de publicación
2023
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Climate change is characterized by global surface warming associated with the increase of greenhouse gas population since the start of the industrial era. Growing evidence shows that the upper atmosphere is experiencing appreciable cooling over the last several decades. The seminal modeling study by Roble and Dickinson (1989) suggested potential effects of increased greenhouse gases on the ionosphere and thermosphere cooling which appear consistent with some observations. However, several outstanding issues remain regarding the role of CO2 , other important contributors, and impacts of the cooling trend in the ionosphere and thermosphere: for example, (1) what is the regional variability of the trends? (2) the very strong ionospheric cooling observed by multiple incoherent scatter radars that does not fit with the prevailing theory based on the argument of anthropogenic greenhouse gas increases, why? (3) what is the effect of secular changes in Earth’s main magnetic field? Is it visible now in the ionospheric data and can it explain some of the regional variability in the observed ionospheric trends? (4) what is the impact of long-term cooling in the thermosphere on operational systems? (5) what are the appropriate strategic plans to ensure the long-term monitoring of the critical space climate?
Fil: Zhang, Shun-Rong. Massachusetts Institute of Technology; Estados Unidos
Fil: Cnossen, Ingrid. British Antartic Survey; Reino Unido
Fil: Laštovička, Jan. Czech Academy of Sciences; República Checa
Fil: Elias, Ana Georgina. Universidad Nacional de Tucumán. Instituto de Física del Noroeste Argentino. - Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet Noa Sur. Instituto de Física del Noroeste Argentino; Argentina
Fil: Yue, Xinan. Chinese Academy of Sciences; República de China
Fil: Jacobi, Christoph. Universitat Leipzig; Alemania
Fil: Yue, Jia. National Aeronautics and Space Administration; Estados Unidos. Catholic University of America; Estados Unidos
Fil: Wang, Wenbin. High Altitude Observatory; Estados Unidos
Fil: Qian, Liying. High Altitude Observatory; Estados Unidos
Fil: Goncharenko, Larisa. Massachusetts Institute of Technology; Estados Unidos
Materia
Long-term trends
Climate
Ionosphere
Geospace
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/243491
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Long-term geospace climate monitoringZhang, Shun-RongCnossen, IngridLaštovička, JanElias, Ana GeorginaYue, XinanJacobi, ChristophYue, JiaWang, WenbinQian, LiyingGoncharenko, LarisaLong-term trendsClimateIonosphereGeospacehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Climate change is characterized by global surface warming associated with the increase of greenhouse gas population since the start of the industrial era. Growing evidence shows that the upper atmosphere is experiencing appreciable cooling over the last several decades. The seminal modeling study by Roble and Dickinson (1989) suggested potential effects of increased greenhouse gases on the ionosphere and thermosphere cooling which appear consistent with some observations. However, several outstanding issues remain regarding the role of CO2 , other important contributors, and impacts of the cooling trend in the ionosphere and thermosphere: for example, (1) what is the regional variability of the trends? (2) the very strong ionospheric cooling observed by multiple incoherent scatter radars that does not fit with the prevailing theory based on the argument of anthropogenic greenhouse gas increases, why? (3) what is the effect of secular changes in Earth’s main magnetic field? Is it visible now in the ionospheric data and can it explain some of the regional variability in the observed ionospheric trends? (4) what is the impact of long-term cooling in the thermosphere on operational systems? (5) what are the appropriate strategic plans to ensure the long-term monitoring of the critical space climate?Fil: Zhang, Shun-Rong. Massachusetts Institute of Technology; Estados UnidosFil: Cnossen, Ingrid. British Antartic Survey; Reino UnidoFil: Laštovička, Jan. Czech Academy of Sciences; República ChecaFil: Elias, Ana Georgina. Universidad Nacional de Tucumán. Instituto de Física del Noroeste Argentino. - Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet Noa Sur. Instituto de Física del Noroeste Argentino; ArgentinaFil: Yue, Xinan. Chinese Academy of Sciences; República de ChinaFil: Jacobi, Christoph. Universitat Leipzig; AlemaniaFil: Yue, Jia. National Aeronautics and Space Administration; Estados Unidos. Catholic University of America; Estados UnidosFil: Wang, Wenbin. High Altitude Observatory; Estados UnidosFil: Qian, Liying. High Altitude Observatory; Estados UnidosFil: Goncharenko, Larisa. Massachusetts Institute of Technology; Estados UnidosFrontiers Media2023-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/243491Zhang, Shun-Rong; Cnossen, Ingrid; Laštovička, Jan; Elias, Ana Georgina; Yue, Xinan; et al.; Long-term geospace climate monitoring; Frontiers Media; Frontiers in Astronomy and Space Sciences; 10; 2-2023; 1-52296-987XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.frontiersin.org/articles/10.3389/fspas.2023.1139230/fullinfo:eu-repo/semantics/altIdentifier/doi/10.3389/fspas.2023.1139230info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:01:48Zoai:ri.conicet.gov.ar:11336/243491instacron: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:34982025-09-10 13:01:48.835CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Long-term geospace climate monitoring
title Long-term geospace climate monitoring
spellingShingle Long-term geospace climate monitoring
Zhang, Shun-Rong
Long-term trends
Climate
Ionosphere
Geospace
title_short Long-term geospace climate monitoring
title_full Long-term geospace climate monitoring
title_fullStr Long-term geospace climate monitoring
title_full_unstemmed Long-term geospace climate monitoring
title_sort Long-term geospace climate monitoring
dc.creator.none.fl_str_mv Zhang, Shun-Rong
Cnossen, Ingrid
Laštovička, Jan
Elias, Ana Georgina
Yue, Xinan
Jacobi, Christoph
Yue, Jia
Wang, Wenbin
Qian, Liying
Goncharenko, Larisa
author Zhang, Shun-Rong
author_facet Zhang, Shun-Rong
Cnossen, Ingrid
Laštovička, Jan
Elias, Ana Georgina
Yue, Xinan
Jacobi, Christoph
Yue, Jia
Wang, Wenbin
Qian, Liying
Goncharenko, Larisa
author_role author
author2 Cnossen, Ingrid
Laštovička, Jan
Elias, Ana Georgina
Yue, Xinan
Jacobi, Christoph
Yue, Jia
Wang, Wenbin
Qian, Liying
Goncharenko, Larisa
author2_role author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Long-term trends
Climate
Ionosphere
Geospace
topic Long-term trends
Climate
Ionosphere
Geospace
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Climate change is characterized by global surface warming associated with the increase of greenhouse gas population since the start of the industrial era. Growing evidence shows that the upper atmosphere is experiencing appreciable cooling over the last several decades. The seminal modeling study by Roble and Dickinson (1989) suggested potential effects of increased greenhouse gases on the ionosphere and thermosphere cooling which appear consistent with some observations. However, several outstanding issues remain regarding the role of CO2 , other important contributors, and impacts of the cooling trend in the ionosphere and thermosphere: for example, (1) what is the regional variability of the trends? (2) the very strong ionospheric cooling observed by multiple incoherent scatter radars that does not fit with the prevailing theory based on the argument of anthropogenic greenhouse gas increases, why? (3) what is the effect of secular changes in Earth’s main magnetic field? Is it visible now in the ionospheric data and can it explain some of the regional variability in the observed ionospheric trends? (4) what is the impact of long-term cooling in the thermosphere on operational systems? (5) what are the appropriate strategic plans to ensure the long-term monitoring of the critical space climate?
Fil: Zhang, Shun-Rong. Massachusetts Institute of Technology; Estados Unidos
Fil: Cnossen, Ingrid. British Antartic Survey; Reino Unido
Fil: Laštovička, Jan. Czech Academy of Sciences; República Checa
Fil: Elias, Ana Georgina. Universidad Nacional de Tucumán. Instituto de Física del Noroeste Argentino. - Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet Noa Sur. Instituto de Física del Noroeste Argentino; Argentina
Fil: Yue, Xinan. Chinese Academy of Sciences; República de China
Fil: Jacobi, Christoph. Universitat Leipzig; Alemania
Fil: Yue, Jia. National Aeronautics and Space Administration; Estados Unidos. Catholic University of America; Estados Unidos
Fil: Wang, Wenbin. High Altitude Observatory; Estados Unidos
Fil: Qian, Liying. High Altitude Observatory; Estados Unidos
Fil: Goncharenko, Larisa. Massachusetts Institute of Technology; Estados Unidos
description Climate change is characterized by global surface warming associated with the increase of greenhouse gas population since the start of the industrial era. Growing evidence shows that the upper atmosphere is experiencing appreciable cooling over the last several decades. The seminal modeling study by Roble and Dickinson (1989) suggested potential effects of increased greenhouse gases on the ionosphere and thermosphere cooling which appear consistent with some observations. However, several outstanding issues remain regarding the role of CO2 , other important contributors, and impacts of the cooling trend in the ionosphere and thermosphere: for example, (1) what is the regional variability of the trends? (2) the very strong ionospheric cooling observed by multiple incoherent scatter radars that does not fit with the prevailing theory based on the argument of anthropogenic greenhouse gas increases, why? (3) what is the effect of secular changes in Earth’s main magnetic field? Is it visible now in the ionospheric data and can it explain some of the regional variability in the observed ionospheric trends? (4) what is the impact of long-term cooling in the thermosphere on operational systems? (5) what are the appropriate strategic plans to ensure the long-term monitoring of the critical space climate?
publishDate 2023
dc.date.none.fl_str_mv 2023-02
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/11336/243491
Zhang, Shun-Rong; Cnossen, Ingrid; Laštovička, Jan; Elias, Ana Georgina; Yue, Xinan; et al.; Long-term geospace climate monitoring; Frontiers Media; Frontiers in Astronomy and Space Sciences; 10; 2-2023; 1-5
2296-987X
CONICET Digital
CONICET
url http://hdl.handle.net/11336/243491
identifier_str_mv Zhang, Shun-Rong; Cnossen, Ingrid; Laštovička, Jan; Elias, Ana Georgina; Yue, Xinan; et al.; Long-term geospace climate monitoring; Frontiers Media; Frontiers in Astronomy and Space Sciences; 10; 2-2023; 1-5
2296-987X
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.frontiersin.org/articles/10.3389/fspas.2023.1139230/full
info:eu-repo/semantics/altIdentifier/doi/10.3389/fspas.2023.1139230
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Frontiers Media
publisher.none.fl_str_mv Frontiers Media
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
_version_ 1842979974383927296
score 12.993085

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