The Structure and Mesoscale Organization of Precipitating Stratocumulus

• Published in: Journal of the atmospheric sciences 2008-05, Vol.65 (5), p.1587-1605
• Main Authors: SAVIC-JOVCIC, Verica, STEVENS, Bjorn
• Format: Article
• Language: English
• Subjects: Albedo; Boundary layer; Boundary layers; Clouds; Earth, ocean, space; Evaporation; Exact sciences and technology; External geophysics; Field study; Marine; Meteorology; Physics of the high neutral atmosphere; Precipitation; Research methodology; Topology
• ISSN: 0022-4928; 1520-0469
• DOI: 10.1175/2007jas2456.1

Large-eddy simulations are used to explore the structure and mesoscale organization of precipitating stratocumulus. The simulations incorporate a simple, two-moment, bulk representation of microphysical processes, which by varying specified droplet concentrations allows for comparisons of simulations that do and do not develop precipitation. The boundary layer is represented over a large (25.6 km × 25.6 km) horizontal domain using a relatively fine mesh, thereby allowing for the development of mesoscale circulations while retaining an explicit representation of cloud radiative, dynamical and microphysical interactions on scales much smaller than the dominant eddy scale. Initial conditions are based on measurements made as part of the Second Dynamics and Chemistry of the Marine Stratocumulus field study (DYCOMS-II). The simulations show that precipitation is accompanied by sharp reductions in cloudiness and changes in flow topology. Mesoscale features emerge in all of the simulations but are amplified in the presence of drizzle. A cloud albedo of near 75% in the nonprecipitating simulation is reduced to less than 35% in the precipitating case. The circulation transitions from a well-mixed, stationary stratocumulus layer with closed-cellular cloud planforms to a stationary cumulus-coupled layer, with incipient open-cellular cloud planforms and sustained domain-averaged surface precipitation rates near 1 mm day−1. The drizzling simulations embody many other features of observed precipitating stratocumulus, including elevated cloud tops in regions of precipitation and locally higher values of subcloud equivalent potential temperature. The latter is shown to result from the tendency for precipitating simulations to develop greater thermodynamic gradients in the subcloud layer as well as mesoscale circulations that locate regions of upward motion in the vicinity of precipitating cells.