Add to ORKGTropical precipitation due to deep convection is typically forced in limited area models by specifying the large-scale vertical velocity or vertical advection terms. Since the dominant thermodynamic balance in the tropics i
The properties of equilibrated tropical convection are studied using a cloud-resolving model with la...
Constraining precipitation processes in climate models with observations is crucial to accurately si...
Regional changes of precipitation intensity, convective structure and column water vapor (CWV) in th...
In the tropical atmosphere, there exist regions de-void of active convection even in conditions whic...
Important features of the proposed formulation for precipitating deep turbulent clouds include the a...
Horizontal temperature gradients are small in the tropical atmosphere, as a consequence of the small...
In this paper, the effect of a simple convection scheme on the zonally averaged tropical general cir...
A cloud-resolving model is modified to implement the weak temperature gradient approximation in orde...
Horizontal temperature gradients are small in the tropical atmosphere, as a consequence of the small...
The applicability of a weak temperature gradient (WTG) formulation for the reorganization of tropica...
The LMDZ4 general circulation model is the atmospheric component of the IPSL-CM4 coupled model which...
Ó 2020 American Meteorological Society. Tropical precipitation extremes are expected to strengthen w...
Projections of precipitation extremes in simulations with global climate models are very uncertain i...
A two-column model of the tropical atmosphere is developed. The two columns are kept in buoyancy equ...
Analytic solutions are derived for a convecting atmosphere with mean ascent using a zero-buoyancy bu...
The properties of equilibrated tropical convection are studied using a cloud-resolving model with la...
Constraining precipitation processes in climate models with observations is crucial to accurately si...
Regional changes of precipitation intensity, convective structure and column water vapor (CWV) in th...
In the tropical atmosphere, there exist regions de-void of active convection even in conditions whic...
Important features of the proposed formulation for precipitating deep turbulent clouds include the a...
Horizontal temperature gradients are small in the tropical atmosphere, as a consequence of the small...
In this paper, the effect of a simple convection scheme on the zonally averaged tropical general cir...
A cloud-resolving model is modified to implement the weak temperature gradient approximation in orde...
Horizontal temperature gradients are small in the tropical atmosphere, as a consequence of the small...
The applicability of a weak temperature gradient (WTG) formulation for the reorganization of tropica...
The LMDZ4 general circulation model is the atmospheric component of the IPSL-CM4 coupled model which...
Ó 2020 American Meteorological Society. Tropical precipitation extremes are expected to strengthen w...
Projections of precipitation extremes in simulations with global climate models are very uncertain i...
A two-column model of the tropical atmosphere is developed. The two columns are kept in buoyancy equ...
Analytic solutions are derived for a convecting atmosphere with mean ascent using a zero-buoyancy bu...
The properties of equilibrated tropical convection are studied using a cloud-resolving model with la...
Constraining precipitation processes in climate models with observations is crucial to accurately si...
Regional changes of precipitation intensity, convective structure and column water vapor (CWV) in th...