Strichartz estimates for geophysical fluid equations using Fourier restriction theory

Fuente: arXiv
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Autori principali: Gentil, Corentin, Tabary, Côme
Natura: Preprint
Pubblicazione: 2024
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author Gentil, Corentin
Tabary, Côme
author_facet Gentil, Corentin
Tabary, Côme
contents 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.
format Preprint
id arxiv_https___arxiv_org_abs_2401_09079
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Strichartz estimates for geophysical fluid equations using Fourier restriction theory
Gentil, Corentin
Tabary, Côme
Analysis of PDEs
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.
title Strichartz estimates for geophysical fluid equations using Fourier restriction theory
topic Analysis of PDEs
url https://arxiv.org/abs/2401.09079