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Campo DC | Valor | Idioma |
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dc.rights.license | © 2020 Elsevier Inc. All rights reserved. | - |
dc.contributor.author | Kahanpää, H. | - |
dc.contributor.author | Viúdez Moreiras, Daniel | - |
dc.date.accessioned | 2022-02-09T10:23:20Z | - |
dc.date.available | 2022-02-09T10:23:20Z | - |
dc.date.issued | 2021-05-01 | - |
dc.identifier.citation | Icarus 359: 114207(2021) | es |
dc.identifier.issn | 0019-1035 | - |
dc.identifier.other | https://www.sciencedirect.com/science/article/abs/pii/S0019103520305406 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12666/487 | - |
dc.description | Martian dust devils are studied by in-situ wind, pressure, and UV data. A methodology for fitting a mathematical vortex model to the data is presented. Clockwise and counterclockwise rotating vortices are equally common. The dust devils prefer relatively flat terrain. Martian dust devils appear to lift dust not only by wind stress. | es |
dc.description.abstract | NASA's Mars Science Laboratory rover Curiosity (MSL) has measured simultaneous fluctuations in wind and atmospheric pressure caused by passing convective vortices, i.e. dustless dust devils. We study the dynamics of these vortices by fitting a mathematical vortex model to the wind and pressure measurements of MSL. The model matches the data adequately well in 29 out of the 33 studied vortex pass events having sufficient data quality. Clockwise and counterclockwise rotating directions are equally common among the studied convective vortices. The vortices seem to prefer certain trajectories, e.g. avoiding steep slopes. However, our results show that due to sensitivity constraints of the method, central pressure drops of Martian dust devils can usually not be accurately determined by fitting a theoretical vortex model to simultaneous pressure and wind measurements of a single station. We also present a methodology extension for further constraining the trajectories and the strengths of dust laden vortices (i.e. dust devils), based on concurrent in-situ solar irradiance measurements. We apply this methodology to the only evidently dust laden vortex in our data set and show that its dust lifting capacity is probably based not only on wind stress lifting. | es |
dc.description.sponsorship | The contribution of H. Kahanpaa was funded by The Finnish Cultural Foundation (grant number 00180446). D. Viudez-Moreiras thanks the project ESP2016-79612-C3-1-R funded by Spanish Ministry of Economy and Competiveness (MINECO). In addition, we wish to express our gratitude to J. Gomez-Elvira, J. Torres, S. Navarro, and the REMS and MSL teams for supporting this investigation. Also, we thank the HiRISE team for the data used to generate Figs. 10 and 11. Finally, we wish to thank Ralph D. Lorenz and an anonymous reviewer for constructive feedback. | es |
dc.language.iso | eng | es |
dc.publisher | Elsevier BV | es |
dc.relation | info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2016-79612-C3-1-R/ES/CIENCIA Y TECNOLOGIA DE INSTRUMENTOS ESPACIALES PARA LA CARACTERIZACION DEL AMBIENTE MARCIANO EN MULTIPLES MISIONES DE NASA - II: REMS (FASE E), TWINS (FASE E) Y MEDA (FASE D)/ | - |
dc.subject | Mars | es |
dc.subject | Mars Atmosphere | es |
dc.subject | Dynamics | es |
dc.subject | Meteorology | es |
dc.title | Modelling martian dust devils using in-situ wind, pressure, and UV radiation measurements by Mars Science Laboratory | es |
dc.type | info:eu-repo/semantics/article | es |
dc.contributor.orcid | 0000-0001-9108-186X | - |
dc.identifier.doi | 10.1016/j.icarus.2020.114207 | - |
dc.identifier.e-issn | 1090-2643 | - |
dc.contributor.funder | Agencia Estatal de Investigación (AEI) | - |
dc.description.peerreviewed | Peerreview | es |
dc.type.hasVersion | info:eu-repo/semantics/publishedVersion | - |
dc.rights.accessRights | info:eu-repo/semantics/restrictedAccess | - |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | - |
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