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dc.rights.license© 2022. The Authors.es
dc.contributor.authorLemmon, M. T.es
dc.contributor.authorSmith, M. D.es
dc.contributor.authorViúdez Moreiras, Danieles
dc.contributor.authorDe la Torre Juarez, M.es
dc.contributor.authorVicente Retortillo, Á.es
dc.contributor.authorMunguira, A.es
dc.contributor.authorSánchez Lavega, A.es
dc.contributor.authorHueso, R.es
dc.contributor.authorMartínez, Germánes
dc.contributor.authorChide, B.es
dc.contributor.authorSullivan, R.es
dc.contributor.authorToledo, D.es
dc.contributor.authorTamppari, L. K.es
dc.contributor.authorBertrand, T.es
dc.contributor.authorBell, J. F.es
dc.contributor.authorNewman, C. E.es
dc.contributor.authorBaker, M.es
dc.contributor.authorBanfield, D.es
dc.contributor.authorRodríguez Manfredi, J. A.es
dc.contributor.authorMaki, Justin N.es
dc.contributor.authorApéstigue, V.es
dc.contributor.otherCentro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y CSIC, MDM-2017-0737es
dc.date.accessioned2023-03-06T12:49:21Z-
dc.date.available2023-03-06T12:49:21Z-
dc.date.issued2022-11-16-
dc.identifier.citationGeophysical Research Letters 49(17): e2022GL100126(2022)es
dc.identifier.issn1944-8007-
dc.identifier.otherhttps://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022GL100126es
dc.identifier.urihttp://hdl.handle.net/20.500.12666/842-
dc.description.abstractRovers and landers on Mars have experienced local, regional, and planetary-scale dust storms. However, in situ documentation of active lifting within storms has remained elusive. Over 5–11 January 2022 (LS 153°–156°), a dust storm passed over the Perseverance rover site. Peak visible optical depth was ∼2, and visibility across the crater was briefly reduced. Pressure amplitudes and temperatures responded to the storm. Winds up to 20 m s−1 rotated around the site before the wind sensor was damaged. The rover imaged 21 dust-lifting events—gusts and dust devils—in one 25-min period, and at least three events mobilized sediment near the rover. Rover tracks and drill cuttings were extensively modified, and debris was moved onto the rover deck. Migration of small ripples was seen, but there was no large-scale change in undisturbed areas. This work presents an overview of observations and initial results from the study of the storm.es
dc.description.sponsorshipThe authors acknowledge and thank the Mars 2020 team. The research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (80NM0018D0004). ML is supported by contract 15–712 from Arizona State University and 1607215 from Caltech-JPL. Funding for some Spain-based co-authors was provided by the Spanish Ministry of Economy and Competitiveness, through the projects No. ESP2014-54256-C4--4R and AYA2015-65041-P; Ministry of Science, Innovation and Universities, projects No. ESP2016-79612-C3-3R, ESP2016-80320-C2-1-R, RTI2018-098728-B- C33 and RTI2018-099825-B-C31; Instituto Nacional de Técnica Aeroespacial; Ministry of Science and Innovation's Centre for the Development of Industrial Technology; Grupos Gobierno Vasco IT1366-19; and European Research Council Consolidator Grant No. 818602. ASL, RH and AMR were supported by grant PID2019-109467GB-I00 funded by MCIN/AEI/10.13039/501100011033/and by Grupos Gobierno Vasco IT1366-19. A. V.-R. is supported by the Spanish State Research Agency (AEI) Project No. MDM-2017-0737 Unidad de Excelencia “María de Maeztu”- Centro de Astrobiología (INTA-CSIC). Any opinions, findings and conclusions or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of funding agencies or the Space Science Institute.es
dc.language.isoenges
dc.publisherAGU Advancing Earth and Space Sciencees
dc.relationinfo:eu-repo/grantAgreement/MINECO//ESP2014-54256-C4-4-R/ES/MICROELECTRONICA DE ESPACIO PARA INSTRUMENTACION AMBIENTAL EN MARTE/es
dc.relationinfo:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/AYA2015-65041-P/ES/DINAMICA, NUBES Y AEROSOLES EN ATMOSFERAS PLANETARIAS/es
dc.relationinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016//ESP2016-79612-C3-3-Res
dc.relationinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2016-80320-C2-1-R/ES/INSTRUMENTACION PARA LA INVESTIGACION Y CIENCIA ATMOSFERICA EN SUPERFICIE DE MARTE/es
dc.relationinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-098728-B-C33/ES/INSTRUMENTACION PARA CARACTERIZAR EL ENTORNO MARCIANO EN MISIONES DE LA NASA: SENSORES DE VIENTO PARA MEDA (CONCLUSION DE LAS FASES D Y E)/es
dc.relationinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-099825-B-C31es
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internationales
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/es
dc.subjectMartian dust stormses
dc.subjectMARS Perseverancees
dc.titleDust, Sand, and Winds Within an Active Martian Storm in Jezero Crateres
dc.typeinfo:eu-repo/semantics/articlees
dc.identifier.doi10.1029/2022GL100126-
dc.contributor.funderInstituto Nacional de Técnica Aeroespacial (INTA)es
dc.contributor.funderMinisterio de Ciencia e Innovación (MICINN)es
dc.contributor.funderMinisterio de Economía y Competitividad (MINECO)es
dc.contributor.funderNASA Jet Propulsion Laboratory (JPL)es
dc.contributor.funderArizona State University (ASU)es
dc.contributor.funderEuropean Research Council (ERC)es
dc.contributor.funderAgencia Estatal de Investigación (AEI)es
dc.description.peerreviewedPeerreviewes
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.type.coarhttp://purl.org/coar/resource_type/c_2df8fbb1es
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/818602es
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