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dc.contributor.authorSánchez Lavega, Agustín
dc.contributor.authorGarcía Melendo, E.
dc.contributor.authorLegarreta, J.
dc.contributor.authorHueso, R.
dc.contributor.authorRío Gaztelurrutia, Teresa del
dc.contributor.authorSanz Requena, José Francisco
dc.contributor.authorPérez Hoyos, Santiago
dc.contributor.authorSimon, A. A.
dc.contributor.authorWong, M. H.
dc.contributor.authorSoria, M.
dc.contributor.authorGómez Forrellad, J. M.
dc.contributor.authorBarry, T.
dc.contributor.authorDelcroix, M.
dc.contributor.authorSayanagi, K. M.
dc.contributor.authorBlalock, J. J.
dc.contributor.authorGunnarson, J. L.
dc.contributor.authorDyudina, U.
dc.contributor.authorEwald, S.
dc.date.accessioned2020-05-16T11:23:26Z
dc.date.available2020-05-16T11:23:26Z
dc.date.issued2020
dc.identifier.citationNature Astronomy, 2020, vol. 4. p. 180-187es
dc.identifier.issn2397-3366
dc.identifier.urihttp://uvadoc.uva.es/handle/10324/40870
dc.descriptionProducción Científica
dc.description.abstractSaturn’s convective storms usually fall in two categories. One consists of mid-sized storms ∼2,000 km wide, appearing as irregular bright cloud systems that evolve rapidly, on scales of a few days. The other includes the Great White Spots, planetary-scale giant storms ten times larger than the mid-sized ones, which disturb a full latitude band, enduring several months, and have been observed only seven times since 1876. Here we report a new intermediate type, observed in 2018 in the north polar region. Four large storms with east–west lengths ∼4,000–8,000 km (the first one lasting longer than 200 days) formed sequentially in close latitudes, experiencing mutual encounters and leading to zonal disturbances affecting a full latitude band ∼8,000 km wide, during at least eight months. Dynamical simulations indicate that each storm required energies around ten times larger than mid-sized storms but ∼100 times smaller than those necessary for a Great White Spot. This event occurred at about the same latitude and season as the Great White Spot in 1960, in close correspondence with the cycle of approximately 60 years hypothesized for equatorial Great White Spots.es
dc.format.mimetypeapplication/pdfes
dc.language.isoenges
dc.publisherSpringer
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.titleA complex storm system in Saturn’s north polar atmosphere in 2018es
dc.typeinfo:eu-repo/semantics/articlees
dc.rights.holder© 2020 Springer
dc.identifier.doi10.1038/s41550-019-0914-9es
dc.relation.publisherversionhttps://www.nature.com/articles/s41550-019-0914-9
dc.identifier.publicationfirstpage180es
dc.identifier.publicationissue2es
dc.identifier.publicationlastpage187es
dc.identifier.publicationtitleNature Astronomyes
dc.identifier.publicationvolume4es
dc.peerreviewedSIes
dc.description.projectMinisterio de Economía, Industria y Competitividad - Fondo Europeo de Desarrollo Regional (project AYA2015-65041-P)
dc.description.projectGobierno Vasco (project IT-366-19)
dc.identifier.essn2397-3366es
dc.type.hasVersioninfo:eu-repo/semantics/draftes


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