Observed Scaling in Clouds and Precipitation and Scale Incognizance in Regional to Global Atmospheric Models

• Published in: Journal of climate 2013-12, Vol.26 (23), p.9313-9333
• Main Authors: O’Brien, Travis A., Li, Fuyu, Collins, William D., Rauscher, Sara A., Ringler, Todd D., Taylor, Mark, Hagos, Samson M., Leung, L. Ruby
• Format: Article
• Language: English
• Subjects: Aircraft; Algorithms; Atmosphere; Atmospheric models; Climate change; Climate models; Climatology; Cloud physics; Clouds; Communities; Convection; Convection clouds; Digitization; Earth, ocean, space; Exact sciences and technology; External geophysics; Geophysics. Techniques, methods, instrumentation and models; Mathematical models; Meteorology; Mineral precipitation; Modeling; Modelling; Parameterization; Parametrization; Physics; Precipitation; Resolution; Robustness; Scaling; Simulation; Stratiform clouds; Water in the atmosphere (humidity, clouds, evaporation, precipitation); Weather; Weather forecasting
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-13-00005.1

Observations of robust scaling behavior in clouds and precipitation are used to derive constraints on how partitioning of precipitation should change with model resolution. Analysis indicates that 90%–99% of stratiform precipitation should occur in clouds that are resolvable by contemporary climate models (e.g., with 200-km or finer grid spacing). Furthermore, this resolved fraction of stratiform precipitation should increase sharply with resolution, such that effectively all stratiform precipitation should be resolvable above scales of ∼50 km. It is shown that the Community Atmosphere Model (CAM) and the Weather Research and Forecasting model (WRF) also exhibit the robust cloud and precipitation scaling behavior that is present in observations, yet the resolved fraction of stratiform precipitation actually decreases with increasing model resolution. A suite of experiments with multiple dynamical cores provides strong evidence that this “scale-incognizant” behavior originates in one of the CAM4 parameterizations. An additional set of sensitivity experiments rules out both convection parameterizations, and by a process of elimination these results implicate the stratiform cloud and precipitation parameterization. Tests with the CAM5 physics package show improvements in the resolution dependence of resolved cloud fraction and resolved stratiform precipitation fraction.