{"refrec":{"BRefID":261626,"RR":"<b>Vincent, D.; Karatekin, O.; Vallaeys, V.; Hayes, G; Mastrogiuseppe, M; Notarnicola, C; Dehant, V.; Deleersnijder, E.</b> (2016). Numerical study of tides in Ontario Lacus, a hydrocarbon lake on the surface of the Saturnian moon Titan. <i>Ocean Dynamics 66(4)</i>: 461-482. <a href=\"http://dx.doi.org/10.1007/s10236-016-0926-2\" target=\"_blank\">dx.doi.org/10.1007/s10236-016-0926-2</a>","BEntID":253644,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Ocean Dynamics 66(4)</i>: 461-482. <a href=\"https://dx.doi.org/10.1007/s10236-016-0926-2\" target=\"_blank\">https://dx.doi.org/10.1007/s10236-016-0926-2</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vincent, D.; Karatekin, O.; Vallaeys, V.; Hayes, G; Mastrogiuseppe, M; Notarnicola, C; Dehant, V.; Deleersnijder, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vincent, D. <i>et al.</i>","Englishabstract":"In the context of the emergence of extra-terrestrial oceanography, we adapted an existing oceanographic model, SLIM (www.climate.be/slim), to the conditions of Titan, a moon of Saturn. The tidal response of the largest southern lake at Titan's surface, namely Ontario Lacus, is simulated. SLIM solves the 2D, depth-averaged shallow water equations on an unstructured mesh using the discontinuous Galerkin finite element method, which allows for high spatial resolution wherever needed. The impact of the wind forcing, the bathymetry, and the bottom friction is also discussed. The predicted maximum tidal range is about 0.56 m in the southern part of the lake, which is more than twice as large as the previous estimates (see Tokano, Ocean Dyn 60:(4) 803-817 doi: 10.1007/s10236-010-0285-3 2010)). The patterns and magnitude of the current are also markedly different from those of previous studies: the tidal motion is not aligned with the major axis of the lake and the speed is larger nearshore. Indeed, the main tidal component rotates clockwise in an exact period of one Titan day and the tidal currents can reach 0.046 ms (-1) close to the shores depending on the geometry and the bathymetry. Except for these specific nearshore regions, the current speed is less than 0.02 ms (-1). Circular patterns can be observed offshore, their rotational direction and size varying along the day.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Numerical study of tides in Ontario Lacus, a hydrocarbon lake on the surface of the Saturnian moon Titan","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Ontario Lacus; Tides; Titan; Finite element; Numerical model;Extraterrestrial oceanography","OtherDescriptors":null,"Notes":null,"AnaPub":2016,"MonPub":null,"DateUpdate":"2016-09-29","DateCreate":"2016-09-28","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000373123300001","VABBcode":null,"OpenAcc":0,"DOI":"10.1007/s10236-016-0926-2"},"refs":null,"anarec":{"AnaID":261626,"PubliDate":2016,"Pagination":"461-482","XtraPublOfAnaID":null,"ISBN":null,"Volume":"66","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45486,"SerRR":"Ocean Dynamics. 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