Abstract
AbstractTropical climate model derived by Frierson et al. (Commun Math Sci 2:591–626, 2004) and its modified versions have been investigated in a number of papers [see, e.g., Li and Titi (Discrete Contin Dyn Syst Series A 36(8):4495–4516, 2016), Wan (J Math Phys 57(2):021507, 2016), Ye (J Math Anal Appl 446:307–321, 2017) and more recently Dong et al. (Discrete Contin Dyn Syst Ser B 24(1):211–229, 2019)]. Here, we deal with the 2D tropical climate model with fractional dissipative terms in the equation of the barotropic mode u and in the equation of the first baroclinic mode v of the velocity, but without diffusion in the temperature equation, and we establish a regularity criterion for this system.
Funder
Università degli Studi di Firenze
Publisher
Springer Science and Business Media LLC
Reference30 articles.
1. Adams, R.A., Fournier, J.F.: Sobolev Spaces, 2nd edn. Elsevier/Academic Press, Amsterdam (2003)
2. Alghamdi, A.M., Gala, S., Ragusa, M.A.: On the blow-up criterion for incompressible Stokes-MHD equations. Results Math. 73(3), Art. 110, 6 pp
3. Constantin, P., Foias, C.: Navier–Stokes Equations. The University of Chicago Press, Chicago (1988)
4. Dong, B., Wang, W., Wu, J., Zhang, H.: Global regularity results for the climate model with fractional dissipation. Discrete Contin. Dyn. Syst. Ser. B 24(1), 211–229 (2019)
5. Frierson, D., Majda, A., Pauluis, O.: Large scale dynamics of precipitation fronts in the tropical atmosphere: a novel relaxation limit. Commun. Math. Sci. 2, 591–626 (2004)
Cited by
3 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献