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dc.contributor.authorHernández Bernal, Jorge
dc.contributor.authorSánchez Lavega, Agustín María ORCID
dc.contributor.authorDel Río Gaztelurrutia, María Teresa
dc.contributor.authorHueso Alonso, Ricardo ORCID
dc.contributor.authorCardesín-Moinelo, Alejandro
dc.contributor.authorRavanis, Eleni
dc.contributor.authorDe Burgos-Sierra, Abel
dc.contributor.authorTitov, Dimitri
dc.contributor.authorWood, Simon
dc.date.accessioned2023-12-28T12:24:59Z
dc.date.available2023-12-28T12:24:59Z
dc.date.issued2019-08-13
dc.identifier.citationGeophysical Research Letters, 46(17/18) : 10330-10337 (2019)es_ES
dc.identifier.issn0094-8276
dc.identifier.issn1944-8007
dc.identifier.urihttp://hdl.handle.net/10810/63694
dc.description.abstractWe study the 2018 Martian global dust storm (GDS 2018) over the Southern Polar Region using images obtained by the Visual Monitoring Camera (VMC) on board Mars Express (MEx) during June and July 2018. Dust penetrated into the polar cap region but never covered the cap completely, and its spatial distribution was nonhomogeneous and rapidly changing. However, we detected long but narrow aerosol curved arcs with a length of ~2,000–3,000 km traversing part of the cap and crossing the terminator into the nightside. Tracking discrete dust clouds allowed measurements of their motions that were toward the terminator with velocities up to 100 m/s. The images of the dust projected into the Martian limb show maximum altitudes of ~70 km but with large spatial and temporal variations. We discuss these results in the context of the predictions of a numerical model for dust storm scenario.es_ES
dc.description.sponsorshipThis work has been supported by the Spanish project AYA2015-65041-P (MINECO/FEDER, UE) and Grupos Gobierno Vasco IT-1366-19. J. H. B. was supported by ESA Contract 4000118461/16/ES/JD, Scientific Support for Mars Express Visual Monitoring Camera. We acknowledge support from the Faculty of the European Space Astronomy Centre (ESAC). VMC raw images used in this study can be accessed through VMC raw file gallery http://blogs.esa.int/ftp/. VMC raw and calibrated images will be available in ESA PSA in the near future. A list of observations used in this paper is provided in the supporting information. MCD database files are available in http://www-mars.lmd.jussieu.fr/mars.html.es_ES
dc.language.isoenges_ES
dc.publisherAGUes_ES
dc.relationinfo:eu-repo/grantAgreement/MINECO/AYA2015-65041-Pes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.subjectMarses_ES
dc.subjectdust stormses_ES
dc.subjectPolar regionses_ES
dc.titleThe 2018 Martian Global Dust Storm over the South Polar Region studied with MEx/VMCes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holder©2019. American Geophysical Union. All Rights Reserved.es_ES
dc.relation.publisherversionhttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2019GL084266es_ES
dc.identifier.doi10.1029/2019GL084266
dc.departamentoesFísica aplicada Ies_ES
dc.departamentoeuFisika aplikatua Ies_ES


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