Clouds and Convective Self‐Aggregation in a Multimodel Ensemble of Radiative‐Convective Equilibrium Simulations [PDF]
The Radiative‐Convective Equilibrium Model Intercomparison Project (RCEMIP) is an intercomparison of multiple types of numerical models configured in radiative‐convective equilibrium (RCE).
Allison A. Wing +40 more
doaj +15 more sources
Congestus Mode Invigoration by Convective Aggregation in Simulations of Radiative‐Convective Equilibrium [PDF]
This study examines how the congestus mode of tropical convection is expressed in numerical simulations of radiative‐convective equilibrium (RCE). We draw insights from the ensemble of cloud‐resolving models participating in the RCE Model Intercomparison
Adam B. Sokol, Dennis L. Hartmann
doaj +4 more sources
Factors determining tropical upper-level cloud radiative effect in the radiative-convective equilibrium framework [PDF]
Investigation of the major factors determining tropical upper-level cloud radiative effect (TUCRE) is crucial for understanding cloud feedback mechanisms.
Hyoji Kang +2 more
doaj +4 more sources
Radiative–convective equilibrium model intercomparison project [PDF]
RCEMIP, an intercomparison of multiple types of models configured in radiative–convective equilibrium (RCE), is proposed. RCE is an idealization of the climate system in which there is a balance between radiative cooling of the atmosphere and heating ...
A. A. Wing +5 more
doaj +6 more sources
Simulations of Radiative‐Convective‐Dynamical Equilibrium
Small‐domain cloud‐resolving model and single‐column model simulations have historically applied one of three representations of large‐scale vertical motion, wLS.
Robert A. Warren +2 more
doaj +2 more sources
Increases in moist‐convective updraught velocities with warming in radiative‐convective equilibrium [PDF]
The scaling of updraught velocities over a wide range of surface temperatures is investigated in simulations of radiative‐convective equilibrium with a cloud‐system resolving model. The updraught velocities increase with warming, with the largest fractional increases occurring in the upper troposphere and for the highest percentile updraughts.
Singh, Martin Simran, O'Gorman, Paul
openaire +5 more sources
Temperature‐Dependence of the Clear‐Sky Feedback in Radiative‐Convective Equilibrium [PDF]
Abstract We quantify the temperature‐dependence of the clear‐sky climate sensitivity in a one‐dimensional radiative‐convective equilibrium model. The atmosphere is adjusted to fixed surface temperatures between 280 and 330 K while preserving other boundary conditions in particular the relative humidity and the CO
Kluft, Lukas +4 more
openaire +3 more sources
Properties, Changes, and Controls of Deep‐Convecting Clouds in Radiative‐Convective Equilibrium
Changes in tropical high clouds associated with deep convection with warming are one of the largest sources of uncertainty in climate feedbacks. Here, we leverage an ensemble of models of many types in an idealized configuration to investigate how and ...
Catherine L. Stauffer, Allison A. Wing
doaj +2 more sources
In this study, the vertical resolution dependency of the high‐cloud fraction response on the increase in sea surface temperature was investigated via radiative‐convective equilibrium simulations.
Tomoki Ohno, Masaki Satoh, Akira Noda
doaj +2 more sources
This study investigates the mechanisms by which small‐scale turbulence and cloud physics determine the organization of large‐scale convection in radiative‐convective equilibrium (RCE), an idealization of the tropical atmosphere.
Xiaoming Shi, Yiyuan Fan
doaj +2 more sources

