Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars

The two upward-looking Thermal InfraRed Sensor (TIRS) channels from the Mars Environmental Dynamics Analyzer (MEDA) instrument suite on board the Perseverance rover enable the retrieval of total aerosol optical depth (dust plus water ice cloud) above the rover for all observations when TIRS is taken...

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Autores: Smith, Michael D., Martínez Martínez, Germán, Sebastián, E., Lemmon, Mark T., Wolff, Michael J., Apéstigue, Victor, Arruego, I., Toledo, Daniel, Viúdez-Moreiras, Daniel, Rodríguez-Manfredi, José Antonio, Torre Juárez, Manuel de la
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2023
País:España
Recursos:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/412894
Acesso em linha:http://hdl.handle.net/10261/412894
https://api.elsevier.com/content/abstract/scopus_id/85147125839
Access Level:acceso abierto
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spelling Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, MarsSmith, Michael D.Martínez Martínez, GermánSebastián, E.Lemmon, Mark T.Wolff, Michael J.Apéstigue, VictorArruego, I.Toledo, DanielViúdez-Moreiras, DanielRodríguez-Manfredi, José AntonioTorre Juárez, Manuel de laThe two upward-looking Thermal InfraRed Sensor (TIRS) channels from the Mars Environmental Dynamics Analyzer (MEDA) instrument suite on board the Perseverance rover enable the retrieval of total aerosol optical depth (dust plus water ice cloud) above the rover for all observations when TIRS is taken. Because TIRS observes at thermal infrared wavelengths, the retrievals are possible during both the day and night and thus, they provide an excellent way to monitor both the diurnal and seasonal variations of aerosols above Jezero Crater. A retrieval algorithm has been developed for this purpose and here, we describe that algorithm along with our results for the first 400 sols of the Perseverance mission covering nearly the entire aphelion season as well as a regional dust storm and the beginning of the perihelion season. We find systematic diurnal variations in aerosol optical depth that can be associated with dust and water ice clouds as well as a clear change from a cloud-filled aphelion season to a perihelion season where dust is the dominant aerosol. A comparison of retrieved optical depths between TIRS and the SkyCam camera that is also part of MEDA indicates evidence of possible diurnal variations in cloud height or particle size.We especially thank the MEDA team for their efforts in obtaining this remarkable data set. G. Martínez. would like to acknowledge JPL funding from USRA Contract 1638782. E. Sebastián would like to acknowledge funding from the Spanish Plan Estatal de I+D+I (ESP2014-54256-C4-1-R, ESP2015-68281-C4-1-R, ESP2016-79612-C3-1-R, RTI2018-099825-B-C31, and MDM-2017-0737). Portions of this research were carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (80NM0018D0004). The NASA and JPL co-authors acknowledge funding from NASA's Game Changing Development and Space Technology Mission Directorate, NASA's Science Mission Directorate, and the Advanced Exploration Systems Program that resided in the previous Human Exploration and Operations Mission Directorate.Peer reviewedAmerican Geophysical UnionJohn Wiley & SonsUniversities Space Research Association (US)Ministerio de Economía y Competitividad (España)Ministerio de Ciencia, Innovación y Universidades (España)Agencia Estatal de Investigación (España)NASAConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202620262023info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://hdl.handle.net/10261/412894https://api.elsevier.com/content/abstract/scopus_id/85147125839reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/MINECO//ESP2014-54256-C4-1-Rinfo:eu-repo/grantAgreement/MINECO//ESP2015-68281-C4-1-Rinfo:eu-repo/grantAgreement/AEI//ESP2016-79612-C3-1-Rinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-099825-B-C31https://doi.org/10.1029/2022JE007560Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/4128942026-05-22T06:33:51Z
dc.title.none.fl_str_mv Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
title Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
spellingShingle Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
Smith, Michael D.
title_short Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
title_full Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
title_fullStr Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
title_full_unstemmed Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
title_sort Diurnal and Seasonal Variations of Aerosol Optical Depth Observed by MEDA/TIRS at Jezero Crater, Mars
dc.creator.none.fl_str_mv Smith, Michael D.
Martínez Martínez, Germán
Sebastián, E.
Lemmon, Mark T.
Wolff, Michael J.
Apéstigue, Victor
Arruego, I.
Toledo, Daniel
Viúdez-Moreiras, Daniel
Rodríguez-Manfredi, José Antonio
Torre Juárez, Manuel de la
author Smith, Michael D.
author_facet Smith, Michael D.
Martínez Martínez, Germán
Sebastián, E.
Lemmon, Mark T.
Wolff, Michael J.
Apéstigue, Victor
Arruego, I.
Toledo, Daniel
Viúdez-Moreiras, Daniel
Rodríguez-Manfredi, José Antonio
Torre Juárez, Manuel de la
author_role author
author2 Martínez Martínez, Germán
Sebastián, E.
Lemmon, Mark T.
Wolff, Michael J.
Apéstigue, Victor
Arruego, I.
Toledo, Daniel
Viúdez-Moreiras, Daniel
Rodríguez-Manfredi, José Antonio
Torre Juárez, Manuel de la
author2_role author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Universities Space Research Association (US)
Ministerio de Economía y Competitividad (España)
Ministerio de Ciencia, Innovación y Universidades (España)
Agencia Estatal de Investigación (España)
NASA
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
description The two upward-looking Thermal InfraRed Sensor (TIRS) channels from the Mars Environmental Dynamics Analyzer (MEDA) instrument suite on board the Perseverance rover enable the retrieval of total aerosol optical depth (dust plus water ice cloud) above the rover for all observations when TIRS is taken. Because TIRS observes at thermal infrared wavelengths, the retrievals are possible during both the day and night and thus, they provide an excellent way to monitor both the diurnal and seasonal variations of aerosols above Jezero Crater. A retrieval algorithm has been developed for this purpose and here, we describe that algorithm along with our results for the first 400 sols of the Perseverance mission covering nearly the entire aphelion season as well as a regional dust storm and the beginning of the perihelion season. We find systematic diurnal variations in aerosol optical depth that can be associated with dust and water ice clouds as well as a clear change from a cloud-filled aphelion season to a perihelion season where dust is the dominant aerosol. A comparison of retrieved optical depths between TIRS and the SkyCam camera that is also part of MEDA indicates evidence of possible diurnal variations in cloud height or particle size.
publishDate 2023
dc.date.none.fl_str_mv 2023
2026
2026
dc.type.none.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/412894
https://api.elsevier.com/content/abstract/scopus_id/85147125839
url http://hdl.handle.net/10261/412894
https://api.elsevier.com/content/abstract/scopus_id/85147125839
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
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info:eu-repo/grantAgreement/MINECO//ESP2014-54256-C4-1-R
info:eu-repo/grantAgreement/MINECO//ESP2015-68281-C4-1-R
info:eu-repo/grantAgreement/AEI//ESP2016-79612-C3-1-R
info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-099825-B-C31
https://doi.org/10.1029/2022JE007560

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dc.publisher.none.fl_str_mv American Geophysical Union
John Wiley & Sons
publisher.none.fl_str_mv American Geophysical Union
John Wiley & Sons
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
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