Results 1 to 10 of about 1,538 (150)

Clouds and Convective Self‐Aggregation in a Multimodel Ensemble of Radiative‐Convective Equilibrium Simulations [PDF]

Journal of Advances in Modeling Earth Systems, 2020
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, Catherine L. Stauffer, Tobias Becker, Kevin A. Reed, Min‐Seop Ahn, Nathan P. Arnold, Sandrine Bony, Mark Branson, George H. Bryan, Jean‐Pierre Chaboureau, Stephan R. De Roode, Kulkarni Gayatri, Cathy Hohenegger, I‐Kuan Hu, Fredrik Jansson, Todd R. Jones, Marat Khairoutdinov, Daehyun Kim, Zane K. Martin, Shuhei Matsugishi, Brian Medeiros, Hiroaki Miura, Yumin Moon, Sebastian K. Müller, Tomoki Ohno, Max Popp, Thara Prabhakaran, David Randall, Rosimar Rios‐Berrios, Nicolas Rochetin, Romain Roehrig, David M. Romps, James H. Ruppert Jr., Masaki Satoh, Levi G. Silvers, Martin S. Singh, Bjorn Stevens, Lorenzo Tomassini, Chiel C. van Heerwaarden, Shuguang Wang, Ming Zhao   +40 more
doaj   +20 more sources

Congestus Mode Invigoration by Convective Aggregation in Simulations of Radiative‐Convective Equilibrium [PDF]

Journal of Advances in Modeling Earth Systems, 2022
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

Simulations of Radiative‐Convective‐Dynamical Equilibrium

Journal of Advances in Modeling Earth Systems, 2020
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, Martin S. Singh, Christian Jakob   +2 more
doaj   +2 more sources

The Impact of a Land‐Sea Contrast on Convective Aggregation in Radiative‐Convective Equilibrium

Journal of Advances in Modeling Earth Systems, 2023
Convective aggregation is an important atmospheric phenomenon which frequently occurs in idealized models in radiative‐convective equilibrium (RCE), where the effects of land, rotation, sea surface temperature gradients, and the diurnal cycle are often ...
Beth Dingley, Guy Dagan, Philip Stier, Ross Herbert   +3 more
doaj   +2 more sources

Radiative–convective equilibrium model intercomparison project [PDF]

Geoscientific Model Development, 2018
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, K. A. Reed, M. Satoh, B. Stevens, S. Bony, T. Ohno   +5 more
doaj   +3 more sources

Factors determining tropical upper-level cloud radiative effect in the radiative-convective equilibrium framework [PDF]

Scientific Reports
Investigation of the major factors determining tropical upper-level cloud radiative effect (TUCRE) is crucial for understanding cloud feedback mechanisms.
Hyoji Kang, Yong-Sang Choi, Jonathan H. Jiang   +2 more
doaj   +2 more sources

Increases in moist‐convective updraught velocities with warming in radiative‐convective equilibrium [PDF]

Quarterly Journal of the Royal Meteorological Society, 2015
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.
Martin S Singh, Paul A O'Gorman
exaly   +4 more sources

Temperature‐Dependence of the Clear‐Sky Feedback in Radiative‐Convective Equilibrium [PDF]

Geophysical Research Letters, 2021
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
Lukas Kluft, Sally Dacie, Manfred Brath   +2 more
exaly   +2 more sources

Fine Vertical Resolution Radiative‐Convective Equilibrium Experiments: Roles of Turbulent Mixing on the High‐Cloud Response to Sea Surface Temperatures

Journal of Advances in Modeling Earth Systems, 2019
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

Sensitivity of the Horizontal Scale of Convective Self‐Aggregation to Sea Surface Temperature in Radiative Convective Equilibrium Experiments Using a Global Nonhydrostatic Model

Journal of Advances in Modeling Earth Systems, 2022
We conduct radiative convection equilibrium experiments using a global nonhydrostatic model to investigate the dependence of convective self‐aggregation (CSA) on domain size and sea surface temperature (SST).
Shuhei Matsugishi, Masaki Satoh
doaj   +2 more sources