TY - JOUR

T1 - Nonsingular surface quasi-geostrophic flow

AU - Constantin, Peter

AU - Nie, Qing

AU - Schörghofer, Norbert

N1 - Funding Information:
We are greatly indebtedt o R. Clelland, D. Cordoba, L. Kadanoff, D. Lohse, A. Malagoli, R. Pierrehum-bert, V. Putkaradze,a nd E. Tabak for discussion. This work was supportedb y NSF, ONR, DOE, and by MR-SEC at The University of Chicago. This researchu sed resourceso f the National Energy Research Scientific Computing Center, which is supportedb y the Office of Energy Researcho f the U.S. Departmento f Energy.

PY - 1998/4/27

Y1 - 1998/4/27

N2 - The dynamics of large eddies in the atmosphere and oceans is described by the surface quasi-geostrophic equation, which is reminiscent of the Euler equations. Thermal fronts build up rapidly. Two different numerical methods combined with analytical criteria are used to show there are no singularities in finite time.

AB - The dynamics of large eddies in the atmosphere and oceans is described by the surface quasi-geostrophic equation, which is reminiscent of the Euler equations. Thermal fronts build up rapidly. Two different numerical methods combined with analytical criteria are used to show there are no singularities in finite time.

KW - Active scalar

KW - Quasi-geostrophic

KW - Singularities

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U2 - 10.1016/S0375-9601(98)00108-X

DO - 10.1016/S0375-9601(98)00108-X

M3 - Article

AN - SCOPUS:0000579087

VL - 241

SP - 168

EP - 172

JO - Physics Letters, Section A: General, Atomic and Solid State Physics

JF - Physics Letters, Section A: General, Atomic and Solid State Physics

SN - 0375-9601

IS - 3

ER -