Abstract

In this paper, we consider the initial-boundary value problem for the two-dimensional primitive equations of the large-scale oceanic dynamics. These models are often used to predict weather and climate change. Using the differential inequality technique, rigorous a priori bounds of solutions and the continuous dependence on the heat source are established. We show the application of symmetry in mathematical inequalities in practice.

Highlights

  • Primitive equations are very useful models which are often used to study the climate and weather prediction

  • Assuming that all unknown functions are independent of the latitude y, Petcu et al [5] obtained the two-dimensional primitive equations of the ocean from the three-dimensional primitive equations

  • Huang et al [7] studied the two-dimensional primitive equations of large-scale ocean in geophysics driven by degenerate noise

Read more

Summary

Introduction

Primitive equations are very useful models which are often used to study the climate and weather prediction. Huang and Guo [6] considered the two-dimensional primitive equations of large-scale oceanic motion. They obtained the the existence and uniqueness of global strong solutions. The aim of this paper is to prove the continuous dependence on the heat source of problem (1)–(3) by using the energy methods. This type of study is devoted to know whether a small change in the equation can cause a large change in the solutions.

Preliminaries of the Problem
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call