This data set contains the simulation outputs used in the study summarized below: We study the cloud response to a +4K surface warming in a new multiscale climate model that uses enough interior resolution to begin explicitly resolving boundary layer turbulence (i.e., ultraparameterization or UP). UP's predictions are compared against those from standard superparameterization (SP). The mean cloud radiative effect feedback turns out to be remarkably neutral across all of our simulations, despite some radical changes in both cloud microphysical parameter settings and cloud‐resolving model grid resolution. The overall low cloud response to warming is a positive low cloud feedback over land, a negative feedback (driven by cloud optical depth i...
Five-year simulation experiments with a multi-scale modeling Framework (MMF) with a advanced interme...
A linear analysis is applied to a multi-thousand member "perturbed physics" GCM ensemble to identify...
Cloud properties and their evolution influence Earth's radiative balance. The cloud microphysical (C...
Systematic biases in the representation of boundary layer (BL) clouds are a leading source of uncert...
Comparative studies of global climate models have long shown a marked sensitivity to the parameteriz...
To test the impact of modeling uncertainties and biases on the simulation of cloud feedbacks, severa...
Using five climate model simulations of the response to an abrupt quadrupling of CO2, the authors pe...
Thesis (Master's)--University of Washington, 2017-03Global climate models (GCMs) with conventional c...
How subtropical marine boundary layer (MBL) clouds respond to warming is investigated using large-ed...
The subtropical low cloud response to a climate with SST uniformly warmed by 2 K is analyzed in the ...
Subtropical marine low cloud sensitivity to an idealized climate change is compared in six large-edd...
Global climate model predictions of future warming vary substantially due to uncertainties in how cl...
For the current generation of climate models, climate response varies from model to model even when ...
International audienceThe response of low-level clouds to climate change has been identified as a ma...
Data from the Tropical Warm Pool International Cloud Experiment (TWP-ICE) were used to evaluate Weat...
Five-year simulation experiments with a multi-scale modeling Framework (MMF) with a advanced interme...
A linear analysis is applied to a multi-thousand member "perturbed physics" GCM ensemble to identify...
Cloud properties and their evolution influence Earth's radiative balance. The cloud microphysical (C...
Systematic biases in the representation of boundary layer (BL) clouds are a leading source of uncert...
Comparative studies of global climate models have long shown a marked sensitivity to the parameteriz...
To test the impact of modeling uncertainties and biases on the simulation of cloud feedbacks, severa...
Using five climate model simulations of the response to an abrupt quadrupling of CO2, the authors pe...
Thesis (Master's)--University of Washington, 2017-03Global climate models (GCMs) with conventional c...
How subtropical marine boundary layer (MBL) clouds respond to warming is investigated using large-ed...
The subtropical low cloud response to a climate with SST uniformly warmed by 2 K is analyzed in the ...
Subtropical marine low cloud sensitivity to an idealized climate change is compared in six large-edd...
Global climate model predictions of future warming vary substantially due to uncertainties in how cl...
For the current generation of climate models, climate response varies from model to model even when ...
International audienceThe response of low-level clouds to climate change has been identified as a ma...
Data from the Tropical Warm Pool International Cloud Experiment (TWP-ICE) were used to evaluate Weat...
Five-year simulation experiments with a multi-scale modeling Framework (MMF) with a advanced interme...
A linear analysis is applied to a multi-thousand member "perturbed physics" GCM ensemble to identify...
Cloud properties and their evolution influence Earth's radiative balance. The cloud microphysical (C...