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dc.contributor.authorMäättänen, Anni E.
dc.contributor.authorFedorova, A.
dc.contributor.authorGiuranna, M.
dc.contributor.authorHernández Bernal, Jorge
dc.contributor.authorLeseigneur, Yann
dc.contributor.authorMontmessin, Franck
dc.contributor.authorOlsen, Kevin
dc.contributor.authorSánchez Lavega, Agustín María ORCID
dc.contributor.authorStcherbinine, A.
dc.contributor.authorSzantai, André
dc.contributor.authorTirsch, Daniela
dc.contributor.authorVincendon, Mathieu
dc.contributor.authorWillame, Yannick
dc.contributor.authorWolkenberg, Paulina
dc.date.accessioned2024-10-02T16:21:43Z
dc.date.available2024-10-02T16:21:43Z
dc.date.issued2024
dc.identifier.citationSpace Science Reviews 220 : (2024) // Article ID 63es_ES
dc.identifier.issn0038-6308
dc.identifier.issn1572-9672
dc.identifier.urihttp://hdl.handle.net/10810/69641
dc.description.abstractEuropean Space Agency’s Mars Express (MEX) has been orbiting Mars for 20 years and its instruments have provided a plethora of observations of atmospheric dust and clouds. These observations have been analysed to produce many unique views of the processes leading to dust lifting and cloud formation, and a full picture of the climatologies of dust and clouds has emerged. Moreover, the orbit of MEX enables viewing the planet at many local times, giving a unique access to the diurnal variations of the atmosphere. This article provides an overview of the observations of dust and clouds on Mars by MEX, complemented by the Trace Gas Orbiter that has been accompanying MEX on orbit for some years.es_ES
dc.description.sponsorshipThe authors thank the International Space Science Institute (ISSI) in Bern, Switzerland for the support. Parts of the studies presented in this paper received funding from the European Union’s Horizon 2020 Programme (H2020-COMPET-08-2014) under grant agreement UPWARDS-633127. ASL was supported by Grupos Gobierno Vasco IT1742-22 and by Grant PID2019-109467GB-I00 funded by MCIN/AEI/10.13039/501100011033/. JHB was supported by ESA Contract No. 4000118461/16/ES/ JD, Scientific Support for Mars Express. KSO was supported by the UK Space Agency (ST/T002069/1 and ST/Y000196/1). The PFS experiment was built at the Institute for Space Astrophysics and Planetology (IAPS) of the National Institute for Astrophysics (INAF), and is currently funded by the Italian Space Agency (ASI; agreement number 2018-2-HH.0). The French authors thank support from the French Space Agency CNES. The authors thank the Belgian Science Policy Office (BELSPO) with the financial and contractual coordination by the European Space Agency (ESA) PROgramme de Développement d’EXpériences scientifiques (PRODEX) office (PEA 4000103401, 4000121493), and from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 101004052 (RoadMap project). Open access funding provided by Istituto Nazionale di Astrofisica within the CRUI-CARE Agreement.es_ES
dc.language.isoenges_ES
dc.publisherSpringer Naturees_ES
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/633127es_ES
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/101004052es_ES
dc.relationinfo:eu-repo/grantAgreement/MICINN/PID2019-109467GB-I00es_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es/*
dc.subjectMarses_ES
dc.subjectatmospherees_ES
dc.subjectcloudses_ES
dc.subjectmineral dustes_ES
dc.titleDust and Clouds on Mars: The View from Mars Expresses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holder© The Author(s) 2024. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.es_ES
dc.rights.holderAtribución 3.0 España*
dc.relation.publisherversionhttps://link.springer.com/article/10.1007/s11214-024-01092-zes_ES
dc.identifier.doi10.1007/s11214-024-01092-z
dc.contributor.funderEuropean Commission
dc.departamentoesFísica aplicada Ies_ES
dc.departamentoeuFisika aplikatua Ies_ES


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© The Author(s) 2024. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
Except where otherwise noted, this item's license is described as © The Author(s) 2024. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.