Results 1 to 10 of about 1,642 (250)
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 +3 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 +5 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
Clouds, Circulation, and Climate Sensitivity in a Radiative‐Convective Equilibrium Channel Model
Tropical cloud and circulation changes are large sources of uncertainty in future climate change. This problem owes partly to the scale separation between large‐scale tropical dynamics ( ∼104 km) and convective dynamics ( ∼1 km), which generally requires
Timothy W. Cronin, Allison A. Wing
doaj +2 more sources
Atmospheric Instability and Its Associated Oscillations in the Tropics
The interaction between tropical clouds and radiation is studied in the context of the weak temperature gradient approximation, using very low order systems (e.g., a two-column two-layer model) as a zeroth-order approximation.
Xiping Zeng
doaj +1 more source
The emergence of a new wintertime Arctic energy balance regime
The modern Arctic climate during wintertime is characterized by sea-ice cover, a strong surface temperature inversion, and the absence of convection. Correspondingly, the energy balance in the Arctic atmosphere today is dominated by atmospheric radiative
O Miyawaki, T A Shaw, M F Jansen
doaj +1 more source
Vertical Resolution Impacts Explicit Simulation of Deep Convection
The aggregation of tropical convection greatly influences the mean‐state of the atmosphere, altering humidity distributions, total atmospheric radiative cooling, and cloud amounts.
A. M. Jenney +2 more
doaj +1 more source

