Inexorable
发表于 2025-3-28 15:14:55
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
发表于 2025-3-28 19:25:26
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
流出
发表于 2025-3-29 00:50:48
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Ascendancy
发表于 2025-3-29 05:28:19
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碎石头
发表于 2025-3-29 08:15:29
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Ebct207
发表于 2025-3-29 14:16:09
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连系
发表于 2025-3-29 19:31:07
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
发表于 2025-3-29 23:23:11
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
发表于 2025-3-30 03:01:57
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
纯朴
发表于 2025-3-30 05:37:12
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