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Surface quasi-geostrophy
G Lapeyre - Fluids, 2017 - mdpi.com
Oceanic and atmospheric dynamics are often interpreted through potential vorticity, as this
quantity is conserved along the geostrophic flow. However, in addition to potential vorticity …
quantity is conserved along the geostrophic flow. However, in addition to potential vorticity …
Computer-assisted proofs in PDE: a survey
J Gómez-Serrano - SeMA Journal, 2019 - Springer
Computer-assisted proofs in PDE: a survey | SeMA Journal Skip to main content Springer
Nature Link Account Menu Find a journal Publish with us Track your research Search Cart 1.Home …
Nature Link Account Menu Find a journal Publish with us Track your research Search Cart 1.Home …
Singularity formation in the incompressible Euler equation in finite and infinite time
Some classical and recent results on the Euler equations governing perfect (incompressible
and inviscid) fluid motion are collected and reviewed, with some small novelties scattered …
and inviscid) fluid motion are collected and reviewed, with some small novelties scattered …
A maximum principle applied to quasi-geostrophic equations
A Córdoba, D Córdoba - Communications in mathematical physics, 2004 - Springer
We study the initial value problem for dissipative 2D Quasi-geostrophic equations proving
local existence, global results for small initial data in the super-critical case, decay of L p …
local existence, global results for small initial data in the super-critical case, decay of L p …
Global well-posedness for the critical 2D dissipative quasi-geostrophic equation
Global well-posedness for the critical 2D dissipative quasi-geostrophic equation Page 1 DOI:
10.1007/s00222-006-0020-3 Invent. math. 167, 445–453 (2007) Global well-posedness for …
10.1007/s00222-006-0020-3 Invent. math. 167, 445–453 (2007) Global well-posedness for …
Behavior of solutions of 2D quasi-geostrophic equations
We study solutions to the 2D quasi-geostrophic (QGS) equation ∂ θ ∂ t+ u ⋅ ∇ θ+ κ (-Δ)^ α
θ= f and prove global existence and uniqueness of smooth solutions if α∈(12,1; weak …
θ= f and prove global existence and uniqueness of smooth solutions if α∈(12,1; weak …
On the regularity of weak solutions to the magnetohydrodynamic equations
C He, Z **n - Journal of Differential Equations, 2005 - Elsevier
In this paper, we study the regularity of weak solution to the incompressible
magnetohydrodynamic equations. We obtain some sufficient conditions for regularity of …
magnetohydrodynamic equations. We obtain some sufficient conditions for regularity of …
Nonlinear maximum principles for dissipative linear nonlocal operators and applications
We obtain a family of nonlinear maximum principles for linear dissipative nonlocal operators,
that are general, robust, and versatile. We use these nonlinear bounds to provide …
that are general, robust, and versatile. We use these nonlinear bounds to provide …
Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics
C Cao, ES Titi - Annals of Mathematics, 2007 - JSTOR
Global Well-Posedness of the Three-Dimensional Viscous Primitive Equations of Large Scale
Ocean and Atmosphere Dynamics Page 1 Annals of Mathematics, 166 (2007), 245-267 Global …
Ocean and Atmosphere Dynamics Page 1 Annals of Mathematics, 166 (2007), 245-267 Global …
[書籍][B] Mathematical geophysics: An introduction to rotating fluids and the Navier-Stokes equations
JY Chemin, B Desjardins, I Gallagher, E Grenier - 2006 - books.google.com
Aimed at graduate students, researchers and academics in mathematics, engineering,
oceanography, meteorology and mechanics, this text provides a detailed introduction to the …
oceanography, meteorology and mechanics, this text provides a detailed introduction to the …