Generator functions and their applications
Abstract
We had introduced so called generators functions to precisely follow the regularity of analytic solutions of Navier-Stokes equations earlier (see Grenier and Nguyen [Ann. PDE 5 (2019)]. In this short note, we give a short presentation of these generator functions and use them to construct analytic solutions to classical evolution equations, which provides an alternative way to the use of the classical abstract Cauchy-Kovalevskaya theorem (see Asano [Proc. Japan Acad. Ser. A Math. Sci. 64 (1988), pp. 102–105], Baouendi and Goulaouic [Comm. Partial Differential Equations 2 (1977), pp. 1151–1162], Caflisch [Bull. Amer. Math. Soc. (N.S.) 23 (1990), pp. 495–500], Nirenberg [J. Differential Geom. 6 (1972), pp. 561–576], Safonov [Comm. Pure Appl. Math. 48 (1995), pp. 629–637]).
1. Introduction
The general abstract Cauchy-Kovalevskaya theorem has been intensively used to construct analytic solutions to various evolution partial differential equations, including first order hyperbolic and parabolic equations, or Euler and Navier-Stokes equations. We refer for instance to Asano Reference 1, Baouendi and Goulaouic Reference 2, Caflisch Reference 6, Nirenberg Reference 16, Safonov Reference 17, among others. In this short note, we use generators functions as introduced in Reference 8 to obtain existence results for these equations. The results in this paper are not new, but show the versatility and simplicity of use of these generator functions. We believe that the approach could be used on many other equations and provide easy ways to obtain analytic solutions, including those at the large time, and to investigate instabilities.
Let us first introduce generator functions in the particular case of a periodic function on and , For . we introduce the generator function , defined by
in which denotes the Fourier transform of with respect to If . is analytic in , is only defined for small enough up to the analyticity radius of , The results in this note also apply to the case when . with which the above summation is replaced by the integral over , In applications, we may also introduce generator functions depending on multi-variables . that correspond to the analyticity radius of in respectively; see, for instance, ,Reference 8 for the case of boundary layers on the half space .
First note that generator functions are non negative, and that all their derivatives are non negative and non decreasing in Moreover generator functions have very nice properties with respect to algebraic operations and differentiation. Namely they “commute” with the product, the sum and the differentiation, making their use very versatile. .
The use of generator functions are not limited to polynomial operations. Namely, we have
2. An analyticity framework
In this section, we present our analyticity framework to construct analytic solutions via generator functions defined as in Equation 1.1. The main point of the approach is that if satisfies a non linear partial differential equation then satisfies a transport differential inequality; see Equation 2.7. This inequality describes in an acute way how the radius of analyticity shrinks as time goes on, and allows to get analytic bounds on and in particular to bound all its derivatives at the same time. ,
To precise the framework, we consider the following general system of evolution equations
for a vector valued function with , , and , We assume that the function . satisfies
for some constant and some analytic functions For instance, . may be a quadratic polynomial in and in which case , or more generally, , may be of the form for which , (see Lemma 1.2). Note that we do not make any assumption on the hyperbolicity of the system Equation 2.1.
We shall construct solutions in the function space defined by
3. Euler equations
In this section, we apply the previous framework to construct analytic solutions to incompressible Euler equations on or , Namely, we consider .
on (the case is treated similarly). Again, the existence result is classical (see, for instance, Reference 3Reference 4Reference 12Reference 13). The function space is defined in Equation 2.3. We have
4. Comments on other applications
In this section, we briefly highlight two recent applications to the use of generator functions to capture the instability of boundary layers Reference 8 and prove the nonlinear Landau damping Reference 9Reference 10, both of which have a different flavor from the previous short time existence theory. These applications Reference 8Reference 9Reference 10 are a version of the large time Cauchy-Kovalevskaya theorem. The use of generator functions allows us to control all the derivatives uniformly in the small viscosity limit or in the large time limit. In particular, the work Reference 9 provides an elementary proof of the nonlinear Landau damping that was first obtained by Mouhot and Villani Reference 15 for analytic data and by Bedrossian, Masmoudi, and Mouhot Reference 5 for Gevrey data.