標(biāo)題: Titlebook: Cloud-Resolving Modeling of Convective Processes; Shouting Gao,Xiaofan Li Book 20081st edition Springer Science+Business Media B.V. 2008 C [打印本頁(yè)] 作者: 力學(xué) 時(shí)間: 2025-3-21 17:58
書(shū)目名稱Cloud-Resolving Modeling of Convective Processes影響因子(影響力)
書(shū)目名稱Cloud-Resolving Modeling of Convective Processes影響因子(影響力)學(xué)科排名
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書(shū)目名稱Cloud-Resolving Modeling of Convective Processes網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Cloud-Resolving Modeling of Convective Processes被引頻次
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書(shū)目名稱Cloud-Resolving Modeling of Convective Processes讀者反饋
書(shū)目名稱Cloud-Resolving Modeling of Convective Processes讀者反饋學(xué)科排名
作者: scrape 時(shí)間: 2025-3-21 23:47 作者: Locale 時(shí)間: 2025-3-22 02:26
Empirische Forschungsergebnisse,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作者: MAZE 時(shí)間: 2025-3-22 05:54 作者: mettlesome 時(shí)間: 2025-3-22 09:45 作者: 延期 時(shí)間: 2025-3-22 15:24 作者: 延期 時(shí)間: 2025-3-22 20:04
Empirische Forschungsergebnisse,ating tropical hydrological and energy cycles. The dominant diurnal signal is the nocturnal peak in precipitation that occurs in the early morning. The second rainfall peak appears in the early afternoon. The nocturnal rainfall maximum may be primarily caused by the IR cooling or radiational differe作者: neoplasm 時(shí)間: 2025-3-22 21:26 作者: 絕食 時(shí)間: 2025-3-23 03:46
Bedingungen schulischer Rassismuskritik,erature stratification through changing ocean surface heat fluxes. The ocean may affect the atmospheric convection and associated thermodynamic distributions through changing the boundary layer stability. In this chapter, the brief history of coupled modeling studies of air–sea interaction processes作者: Modify 時(shí)間: 2025-3-23 06:17 作者: 來(lái)這真柔軟 時(shí)間: 2025-3-23 11:35
https://doi.org/10.1007/978-3-658-20618-5 important sources that provide atmospheric thermodynamic profiles, cloud properties, and surface parameters, in particular over vast ocean, where conventional observations are not available. Cloud-resolving model simulations can provide vertical profiles of temperature, water vapor, and cloud hydro作者: enlist 時(shí)間: 2025-3-23 15:28
Schulklassen als soziale Netzwerke cloud clusters in the genesis, evolution, propagation, and amplitudes. However, the computation of the full set of prognostic cloud microphysical equations is time-consuming. Thus, simplified prognostic cloud microphysical parameterization schemes are discussed in this chapter. Possible replacement作者: 一回合 時(shí)間: 2025-3-23 21:40
https://doi.org/10.1007/978-1-4020-8276-4Cloud; Precipitation; Rain; Scale; atmosphere; cyclone; spheric作者: 大漩渦 時(shí)間: 2025-3-23 23:31
978-90-481-7829-2Springer Science+Business Media B.V. 2008作者: 發(fā)誓放棄 時(shí)間: 2025-3-24 05:49 作者: aggrieve 時(shí)間: 2025-3-24 06:57 作者: Coronation 時(shí)間: 2025-3-24 12:41
ormation on many research aspects related to convective deve.Clouds and cloud systems and their interactions with larger scales of motion, radiation, and the Earth’s surface are extremely important parts of weather and climate systems. Their treatment in weather forecast and climate models is a sign作者: APEX 時(shí)間: 2025-3-24 15:31
Schulklassen als soziale Netzwerkeations is time-consuming. Thus, simplified prognostic cloud microphysical parameterization schemes are discussed in this chapter. Possible replacement of cumulus parameterization in general circulation models (GCMs) with cloud-resolving model (CRM) package and recent progress in global cloud-resolving modeling are addressed.作者: insular 時(shí)間: 2025-3-24 19:54 作者: phytochemicals 時(shí)間: 2025-3-24 23:44 作者: Irrigate 時(shí)間: 2025-3-25 06:26
https://doi.org/10.1007/978-3-531-90557-0ertical structure of temperature and water vapor anomalies, cloud hydrometeors, and surface rainfall processes before and after merging are compared in this chapter. The surface rainfall processes associated with the development of cloud clusters by Wang et al. (2007) are also discussed.作者: CLAN 時(shí)間: 2025-3-25 10:49 作者: conscribe 時(shí)間: 2025-3-25 13:51
https://doi.org/10.1007/978-3-658-20618-5 contamination from cloudy radiances. Thus, responses of radiance to cloud hydrometeors, correction of cloud contamination on cloudy radiances, and comparison between observed and simulated radiances are discussed in this chapter.作者: 下邊深陷 時(shí)間: 2025-3-25 19:31
Tropical Cloud Clusters,ertical structure of temperature and water vapor anomalies, cloud hydrometeors, and surface rainfall processes before and after merging are compared in this chapter. The surface rainfall processes associated with the development of cloud clusters by Wang et al. (2007) are also discussed.作者: MIRE 時(shí)間: 2025-3-25 20:35 作者: Conquest 時(shí)間: 2025-3-26 00:13 作者: inundate 時(shí)間: 2025-3-26 04:24
Analysis Methodology,sis is an important part of the modeling study towards better understanding of clouds and associated microphysics and thermodynamics and their impacts on tropical hydrological and energy cycles, which is discussed in this chapter.作者: 同時(shí)發(fā)生 時(shí)間: 2025-3-26 10:53 作者: cuticle 時(shí)間: 2025-3-26 13:39 作者: Cerumen 時(shí)間: 2025-3-26 20:29
Schulkultur, Milieu und Individuation,88. In this chapter, a brief history of equilibrium studies with cloud-resolving modeling is reviewed. Effects of ., diurnal variations, and cloud microphysical and radiative processes on tropical equilibrium states are discussed based on Gao et al. (2007), Ping et al. (2007), Cui and Gao (2008), and Gao (2008).作者: 采納 時(shí)間: 2025-3-26 22:04 作者: 混合,攙雜 時(shí)間: 2025-3-27 02:53 作者: floodgate 時(shí)間: 2025-3-27 08:55
Anna Schnitzer,Andrea Bossen,Tanya Tyagunovatwo-dimensional (2D) framework in terms of governing equations, large-scale forcing, parameterization schemes of cloud microphysics, radiation, subgrid-scale turbulence closure, ocean mixing closure, and boundary conditions.作者: 威脅你 時(shí)間: 2025-3-27 12:49 作者: Redundant 時(shí)間: 2025-3-27 16:58 作者: 火花 時(shí)間: 2025-3-27 19:50
Empirische Forschungsergebnisse,ional and numerical studies of diurnal rainfall variations is briefly reviewed. The nocturnal rainfall peak is discussed by analyzing domain mean cloud-resolving model simulation data during TOGA COARE. The nocturnal and afternoon rainfall peaks are examined by analyzing grid data from a coupled oce作者: 袖章 時(shí)間: 2025-3-28 00:45
Rassismuskritische Perspektiven auf Schule, This indicates that some precipitation sources may not be included in the definitions. To fix it, new de- finitions of precipitation efficiency are introduced by Sui et al. (2007), in which the precipitation efficiency is less than or equal to 100%. In this chapter, the definition of precipitation 作者: cluster 時(shí)間: 2025-3-28 03:07 作者: Lipoprotein 時(shí)間: 2025-3-28 08:43 作者: CHOP 時(shí)間: 2025-3-28 12:17 作者: Inexorable 時(shí)間: 2025-3-28 15:14
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作者: Complement 時(shí)間: 2025-3-28 19:25
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作者: 流出 時(shí)間: 2025-3-29 00:50 作者: Ascendancy 時(shí)間: 2025-3-29 05:28 作者: 碎石頭 時(shí)間: 2025-3-29 08:15 作者: Ebct207 時(shí)間: 2025-3-29 14:16 作者: 連系 時(shí)間: 2025-3-29 19:31
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作者: TRAWL 時(shí)間: 2025-3-29 23:23
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作者: 套索 時(shí)間: 2025-3-30 03:01
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作者: 純樸 時(shí)間: 2025-3-30 05:37
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作者: 阻礙 時(shí)間: 2025-3-30 11:17 作者: deforestation 時(shí)間: 2025-3-30 13:39 作者: COW 時(shí)間: 2025-3-30 17:22 作者: 貧困 時(shí)間: 2025-3-30 23:03
Climate Equilibrium States,e and cloud dynamics, cloud microphysics, radiative and surface processes, turbulence, and ocean mixing processes. The cloud-resolving modeling of convective–radiative equilibrium states provides ways to enhance the understanding of these controlling processes. The equilibrium studies with cloud-res
