Hamiltonian formalism for models of rotating shallow water insemigeostrophic scaling

Hamiltonian formalism for models of rotating shallow water insemigeostrophic scaling
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半地转尺度旋转浅水模型的哈密顿形式主义

DOI:
10.3934/dcds.2011.31.827
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发表时间:
2011
影响因子:
1.1
通讯作者:
S. Vasylkevych
S. Vasylkevych
中科院分区:
数学3区
文献类型:
--
作者:
M. Oliver;S. Vasylkevych

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本文首次提出了所谓的严谨研究
This paper presents a first rigorous study of the so-called large-scale semigeostrophic equations which were first introduced by R. Salmon in 1985 and later generalized by the first author. We show that these models are Hamiltonian on the group of $H^s$ diffeomorphisms for $s>2$. Notably, in the Hamiltonian setting an apparent topological restriction on the Coriolis parameter disappears. We then derive the corresponding Hamiltonian formulation in Eulerian variables via Poisson reduction and give a simple argument for the existence of $H^s$ solutions locally in time.