Abstract. Much of the large uncertainty in estimates of an-thropogenic aerosol effects on climate arises from the multi-scale nature of the interactions between aerosols, clouds and dynamics, which are difficult to represent in conventional general circulation models (GCMs). In this study, we use a multi-scale aerosol-climate model that treats aerosols and clouds across multiple scales to study aerosol indirect effects. This multi-scale aerosol-climate model is an extension of a multi-scale modeling framework (MMF) model that embeds a cloud-resolving model (CRM) within each vertical column of a GCM grid. The extension allows a more physically-based treatment of aerosol-cloud interactions in both strat-iform and convective clouds on the glob...
Natural modes of variability on many timescales influence aerosol particle distributions and cloud p...
Aerosols affect the climate system by changing cloud characteristics in many ways. They act as cloud...
The effect of an increase in atmospheric aerosol concentrations on the distribution and radiative pr...
Much of the large uncertainty in estimates of anthropogenic aerosol effects on climate arises from t...
Much of the large uncertainty in estimates of anthropogenic aerosol effects on climate arises from t...
Abstract. Anthropogenic aerosol effects on climate pro-duce one of the largest uncertainties in esti...
Anthropogenic aerosol effects on climate produce one of the largest uncertainties in estimates of ra...
Strategies to detect and attribute aerosol global impacts on clouds and climate from synergetic appr...
Aerosol–cloud interactions continue to constitute a major source of uncertainty for the estimate of ...
The interactions between aerosols and convective clouds represent some of the greatest uncertainties...
One of the biggest uncertainties associated with climate models and climate forcing is the treatment...
Numerical cloud models, which are based the non-hydrostatic equations of motion, have been extensive...
The effect of an increase in atmospheric aerosol concentrations on the distribution and radiative pr...
The effect of an increase in atmospheric aerosol concentrations on the distribution and radiative pr...
In recent years, exponentially increasing computer power has extended Cloud Resolving Model (CRM) in...
Natural modes of variability on many timescales influence aerosol particle distributions and cloud p...
Aerosols affect the climate system by changing cloud characteristics in many ways. They act as cloud...
The effect of an increase in atmospheric aerosol concentrations on the distribution and radiative pr...
Much of the large uncertainty in estimates of anthropogenic aerosol effects on climate arises from t...
Much of the large uncertainty in estimates of anthropogenic aerosol effects on climate arises from t...
Abstract. Anthropogenic aerosol effects on climate pro-duce one of the largest uncertainties in esti...
Anthropogenic aerosol effects on climate produce one of the largest uncertainties in estimates of ra...
Strategies to detect and attribute aerosol global impacts on clouds and climate from synergetic appr...
Aerosol–cloud interactions continue to constitute a major source of uncertainty for the estimate of ...
The interactions between aerosols and convective clouds represent some of the greatest uncertainties...
One of the biggest uncertainties associated with climate models and climate forcing is the treatment...
Numerical cloud models, which are based the non-hydrostatic equations of motion, have been extensive...
The effect of an increase in atmospheric aerosol concentrations on the distribution and radiative pr...
The effect of an increase in atmospheric aerosol concentrations on the distribution and radiative pr...
In recent years, exponentially increasing computer power has extended Cloud Resolving Model (CRM) in...
Natural modes of variability on many timescales influence aerosol particle distributions and cloud p...
Aerosols affect the climate system by changing cloud characteristics in many ways. They act as cloud...
The effect of an increase in atmospheric aerosol concentrations on the distribution and radiative pr...