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Atmospheric Sciences & Global Change
Research Highlights

January 2018

Satellites Illuminate Challenges in Simulating Clouds

Comparisons reveal consistency in climate model deficiencies for low clouds.

marine cloudsMarine boundary layer clouds are important in terms of regulating the Earth's energy balance, but it is difficult to accurately represent these clouds and related physical processes in climate models. The processes occur at much smaller scales than a typical model grid size of about 100 kilometers.

The Science

Low clouds over the ocean surface—known as marine boundary layer clouds—play a critical role in regulating the Earth's energy balance. However, accurately representing these clouds and related physical processes, such as turbulence and convection, in climate models is difficult. These processes occur at much smaller scales than a typical model grid size of about 100 kilometers, so "subgrid" cloud representations are necessary to reliably represent and connect small-scale cloud processes with larger grid-level variables in climate models.

Researchers from the U.S. Department of Energy's Pacific Northwest National Laboratory participated in a study showing a direct relationship between model biases—offsets from satellite observations—in the simulated frequency of very thin, low clouds and of precipitation from those clouds.

The Impact

Model deficiencies identified in this study related to low-cloud frequency and precipitation will guide improvements in representing low clouds and simulating their effects in Earth system models.

Summary

Clouds affect Earth's climate in a variety of ways, including scattering and absorbing energy coming from sunlight and the surface and through precipitation. This study used global satellite data to evaluate two aspects of low clouds (within 1,000 meters of the surface) that are very important for climate: their influence on sunlight and the likelihood that they will produce drizzle or rain.

Researchers evaluated and compared two different model representations of clouds within the Community Atmosphere Model Version 5 (CAM5). Comparing the representations with the satellite observations, researchers found that both representations simulated too many thin, wispy clouds that scatter little sunlight. They also noted that both cloud treatments simulated drizzle far too often. These findings suggest that the excessive drizzle in both cloud representations depletes the water in low clouds and that correcting the drizzle problem will result in more realistic simulations of sunlight scattering.

Acknowledgments

Sponsors: The U.S. Department of Energy Office of Science, Biological and Environmental Research supported this research as part of the Regional and Global Climate Modeling program.

Research Area: Climate and Earth Systems Science

Research Team: Hua Song and Zhibo Zhang, University of Maryland, Baltimore County; Po-Lun Ma and Steven Ghan, PNNL; and Minghuai Wang, Institute for Climate and Global Change Research & School of Atmospheric Sciences, Nanjing University (China)

Reference: H. Song, Z. Zhang, P.-L. Ma, S. Ghan, M. Wang, "An Evaluation of Marine Boundary Layer Cloud Property Simulations in Community Atmosphere Model Using Satellite Observations: Conventional Sub-grid Parameterization vs. CLUBB." Journal of Climate 31, 2299-2320 (2018). [DOI: 10.1175/JCLI-D-17-0277.1]


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