Atmospheric Science
Introducing subgrid-scale cloud feedbacks to radiation for regional meteorological and climate modeling
Article first published online: 21 DEC 2012
DOI: 10.1029/2012GL054031
This paper is not subject to U.S. copyright. Published in 2012 by the American Geophysical Union
Additional Information
How to Cite
, , , , , , , and (2012), Introducing subgrid-scale cloud feedbacks to radiation for regional meteorological and climate modeling, Geophys. Res. Lett., 39, L24809, doi:10.1029/2012GL054031.
Publication History
- Issue published online: 21 DEC 2012
- Article first published online: 21 DEC 2012
- Manuscript Accepted: 14 NOV 2012
- Manuscript Revised: 12 NOV 2012
- Manuscript Received: 26 SEP 2012
Keywords:
- cumulus cloudiness;
- precipitation;
- radiation
[1] Convective systems and associated cloudiness directly influence regional and local atmospheric radiation budgets, as well as dynamics and thermodynamics, through feedbacks. However, most subgrid-scale convective parameterizations in regional weather and climate models do not consider cumulus cloud feedbacks to radiation, resulting in biases in several meteorological parameters. We have incorporated this key feedback process into a convective parameterization and a radiation scheme in the Weather Research and Forecasting model, and evaluated the impacts of including this process in short-term weather and multiyear climate simulations. Introducing subgrid-scale convective cloud-radiation feedbacks leads to a more realistic simulation of attenuation of downward surface shortwave radiation. Reduced surface shortwave radiation moderates the surface forcing for convection and results in a notable reduction in precipitation biases. Our research reveals a need for more in-depth consideration of the effects of subgrid-scale clouds in regional meteorology/climate and air quality models on radiation, photolysis, cloud mixing, and aerosol indirect effects.

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