Abstract. The determination of the large scale boundaries between moist and dry re-gions is an important problem in contemporary meteorology. These phenomena have been addressed recently in a simplified tropical climate model through a novel hyperbolic free boundary formulation yielding three families (drying, slow moistening, and fast moisten-ing) of precipitation fronts. The last two wave types violate Lax’s shock inequalities yet are robustly realized. This formal hyperbolic free boundary problem is given here a rigorous mathematical basis by establishing the existence and uniqueness of suitable weak solutions arising in the zero relaxation limit. A new L2-contraction estimate is also established at positive relaxation values. The goal h...
This book is a survey of the research work done by the author over the last 15 years, in collaborati...
Global Well-posedness for the Primitive Equations Coupled to Nonlinear Moisture Dynamics with Phase ...
The semi-geostrophic equations are an approximate model used to study the large-scale behaviour of t...
In this paper, we consider a nonlinear interaction system between the barotropic mode and the first ...
We study a moisture model for warm clouds that has been used by Klein and Majda (2006 Theor. Comput....
This paper is devoted to reviewing several recent developments concerning certain class of geophysic...
International audienceWe derive a two-layer rotating shallow-water model for a moist atmosphere with...
In this paper, we consider the Cauchy problem to the tropical climate model derived by Frierson-Majd...
In this work we study the global solvability of the primitive equations for the atmosphere coupled t...
Horizontal temperature gradients are small in the tropical atmosphere, as a consequence of the small...
It is well known that the tropical climate model is an important model to describe the interaction o...
In this work we study the global solvability of the primitive equations for the atmosphere coupled t...
The authors present a new model of the tropical surface circulation, forced by changes in sensible h...
Moist idealized baroclinic-wave simulations show the development of precipitation bands from a zonal...
In this paper we deal with the 3D tropical climate model with damping terms in the equation of the b...
This book is a survey of the research work done by the author over the last 15 years, in collaborati...
Global Well-posedness for the Primitive Equations Coupled to Nonlinear Moisture Dynamics with Phase ...
The semi-geostrophic equations are an approximate model used to study the large-scale behaviour of t...
In this paper, we consider a nonlinear interaction system between the barotropic mode and the first ...
We study a moisture model for warm clouds that has been used by Klein and Majda (2006 Theor. Comput....
This paper is devoted to reviewing several recent developments concerning certain class of geophysic...
International audienceWe derive a two-layer rotating shallow-water model for a moist atmosphere with...
In this paper, we consider the Cauchy problem to the tropical climate model derived by Frierson-Majd...
In this work we study the global solvability of the primitive equations for the atmosphere coupled t...
Horizontal temperature gradients are small in the tropical atmosphere, as a consequence of the small...
It is well known that the tropical climate model is an important model to describe the interaction o...
In this work we study the global solvability of the primitive equations for the atmosphere coupled t...
The authors present a new model of the tropical surface circulation, forced by changes in sensible h...
Moist idealized baroclinic-wave simulations show the development of precipitation bands from a zonal...
In this paper we deal with the 3D tropical climate model with damping terms in the equation of the b...
This book is a survey of the research work done by the author over the last 15 years, in collaborati...
Global Well-posedness for the Primitive Equations Coupled to Nonlinear Moisture Dynamics with Phase ...
The semi-geostrophic equations are an approximate model used to study the large-scale behaviour of t...