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arXiv 2401.09079math.AP
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利用 Fourier 限制理论研究地球物理流体方程的 Strichartz 估计

Strichartz estimates for geophysical fluid equations using Fourier restriction theory

Corentin Gentil, Côme Tabary

AI总结:

本文用基于 Tomas-Stein 定理的切片方法和 Fourier 限制理论,证明旋转和/或分层无粘地球物理流体半群的 Strichartz 估计,并在分层情形得到尖锐结果。

摘要:

我们利用 Fourier 限制理论,证明了与分层和/或旋转的无粘地球物理流体相关半群的 Strichartz 估计。我们证明了关于旋转分层流体的新结果,并重新得到了文献[16]中仅旋转情形以及文献[17]中仅分层情形的结果。我们的限制估计通过文献[20]的切片方法获得,该方法依赖于著名的二维球面 Tomas-Stein 定理。据我们所知,这种方法此前从未在此背景下使用。此外,当流体具有分层时,我们的方法给出尖锐估计,表明切片方法捕捉了所关注曲面的全部可用曲率。

英文摘要:

We prove Strichartz estimates for the semigroups associated to stratified and/or rotating inviscid geophysical fluids using Fourier restriction theory. We prove new results for rotating stratified fluids, and recover results from [16] for rotation only, and from [17] for stratification only. Our restriction estimates are obtained by the slicing method [20], which relies on the well-known Tomas-Stein theorem for 2-dimensional spheres. To our knowledge, such a method has never been used in this setting. Moreover, when the fluid is stratified, our approach yields sharp estimates, showing that the slicing method captures all the available curvature of the surfaces of interest.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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