Titlebook: Cloud-Resolving Modeling of Convective Processes; Shouting Gao,Xiaofan Li Book 20081st edition Springer Science+Business Media B.V. 2008 C

Inexorable

Comparison Between Simulations and Observations,tial water vapor conditions and associated physical processes are discussed in this chapter based on Li et al. (2006)..Due to limitations in computational power, the cloud-resolving model simulations have been mainly carried out in the 2D (x–z) framework while the threedimensional (3D) simulations h

Complement

Convective, Moist, and Dynamic Vorticity Vectors,important dynamic concept, has been applied to the study of convective storms in recent decades (e.g., Lilly 1986; Droegemeier et al. 1993; Tan and Wu 1994) since it was introduced by Betchov (1961). However, PV and helicity cannot be applied to the analysis in the 2D framework..Convective (.), mois

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Ascendancy

碎石頭

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連系

Comparison Between Simulations and Observations,ture and moisture, surface fluxes, and precipitation. The evaluation of simulations with observations lays down the foundation for further process studies with cloud-resolving models, aiming towards understanding dynamic, thermodynamic, cloud microphysical processes associated with the development o

TRAWL

Tropical Cloud Clusters,ed within them propagate in different directions and have different evolution and spatial distributions (e.g., Nakazawa 1988; Lau et al. 1991; Sui and Lau 1992). These hierarchical cloud structures and behaviors can be simulated with a 2D cloud-resolving model (e.g., Peng et al. 2001; Ping et al. 20

套索

Cloud Radiative and Microphysical Processes,ion, cloudresolving models resolve individual cloud and simulate cloud radiative and microphysical processes through solar and IR radiative parameterization and prognostic cloud microphysics parameterization. Cloud microphysical processes include vapor condensation and deposition, autoconversion, ev

純樸

Convective, Moist, and Dynamic Vorticity Vectors,nd development of weather systems for more than six decades since it was first introduced by Ertel (1942). PV is conserved in a frictionless, adiabatic flow in a dry atmosphere. Later, moist PV was introduced by replacing potential temperature with the equivalent potential temperature. Moist PV is c