Titlebook: Cloud-Resolving Modeling of Convective Processes; Xiaofan Li,Shouting Gao Book 2016Latest edition Springer International Publishing Switze

皮薩

Structures of Precipitation Systems I: Cloud-Content Analysis, the ratio of ice water path to liquid water path. The tendency equation of the cloud ratio is derived from prognostic equations of mixing ratios of five cloud hydrometeors. The tendency of the cloud ratio is associated with conversion between the ice and liquid water paths, condensation and deposit

detach

Structures of Precipitation Systems II: Budget Analysis,ion systems. The rainfall is separated by atmospheric drying/moistening, water vapor, and hydrometeor convergence/divergence in surface rainfall budget. The rainfall types are combined based on vertical profiles of vertical velocity and major cloud microphysical processes to develop a new technique

Root494

Tropical Cloud Clusters,ation data. The merging processes of cloud clusters are examined in terms of circulations and the composite analysis of total hydrometeor mixing ratio, zonal wind and vertical velocity, temperature and specific humidity perturbations, and surface rainfall budget. A rainfall event during the South Ch

吃掉

硬化

會(huì)犯錯(cuò)誤

Convective, Moist, and Dynamic Vorticity Vectors,valent potential temperature and specific humidity and wind vector, respectively. These vorticity vectors and cloud hydrometeor are highly correlated. The tendency equations of these vorticity vectors are derived to show the linkage between dynamic, thermodynamic, and cloud microphysical processes.

Tortuous

Diurnal Variations of Tropical Oceanic Convection,cal analysis of condensation and deposition shows that diurnal variation of temperature is primarily responsible for that of condensation and deposition. Diurnal variations of convective and stratiform rainfall are also examined based on the analysis of surface rainfall budget.

沉思的魚(yú)

Precipitation Efficiency,, cloud, and rain budgets. The analysis demonstrates that the precipitation efficiency in cloud budget is larger than that in surface rainfall budget, but it is smaller than that in rain budget. Previous studies show precipitation efficiency could be negative or over 100?%. Precipitation efficiency

Charlatan

Air-Sea Coupling,ure, salinity, and depth between 1D and 2D ocean models coupled with cloud-resolving atmosphere model are examined through the analysis of mixed layer heat and salinity budgets. The relationships between rain rate and sea surface temperature and between surface evaporation flux and sea surface tempe

婚姻生活

Climate Equilibrium States,ariation, diurnal variation of radiation, and cloud-radiative and microphysical processes on climate equilibrium states. Heat and water vapor budgets are analyzed to highlight dominant physical processes that are responsible for these effects. The effects of zonal perturbations of sea surface temper