{"refrec":{"BRefID":448454,"RR":"<b>Abdulah, D.; Kang, W.; Rekier, J.</b> (2026). Inertia-gravity wave dissipation and form drag. II. Nontraditional effects. <i>Physical Review Fluids 11(5)</i>: 053802. <a href=\"https://dx.doi.org/10.1103/qy29-8r2t\" target=\"_blank\">https://dx.doi.org/10.1103/qy29-8r2t</a>","BEntID":446292,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Physical Review Fluids 11(5)</i>: 053802. <a href=\"https://dx.doi.org/10.1103/qy29-8r2t\" target=\"_blank\">https://dx.doi.org/10.1103/qy29-8r2t</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Abdulah, D.; Kang, W.; Rekier, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Abdulah, D.; Kang, W.; Rekier, J.","Englishabstract":"The problem of inertia-gravity waves excited by harmonic flow over topography is often simplified by the traditional approximation, which neglects the horizontal component of the Coriolis force. We consider waves forced by a two-dimensional tidal potential in a finite-depth domain, considering the full (nontraditional) Coriolis force, nonhydrostatic effects, and contribution from higher-order harmonics. We provide formulas for the vertical velocity, form drag, and conversion rate of inertia-gravity waves. Overall, including the nontraditional Coriolis force enhances the conversion rate and torque of inertia-gravity waves and extends the range of latitudes that can support them. Inertia-gravity waves under nontraditional rotation exhibit weaker suppression of the conversion rate in the low-depth limit, and weaker nonacoustic effects in the rapidly rotating limit at low latitudes.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Inertia-gravity wave dissipation and form drag. II. 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