Existence of a strong solution to moist atmospheric equations with the effects of topography

Abstract

Abstract In this paper, we consider the primitive three-dimensional viscous equations for large-scale atmosphere dynamics with topography effects and water vapor phase transition process. This modified climate model is commonly used in weather and climate predictions, and few theoretical analyses have been performed on them. The existence and uniqueness of a global strong solution to this climate model is established based on the initial data assumptions.

Keywords

• Climate dynamics
• Strong solution
• Moist atmospheric
• Topography
• Existence