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

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51#
發(fā)表于 2025-3-30 11:11:46 | 只看該作者
52#
發(fā)表于 2025-3-30 14:13:18 | 只看該作者
Precipitation Predictability,n calculations. The effects of large-scale forcing on precipitation predictability is examined by conducting sensitivity experiments with a weak forcing from tropical rainfall event and with a strong forcing from pre-summer torrential rainfall event. The ratio of the root-mean-squared difference bet
53#
發(fā)表于 2025-3-30 16:50:08 | 只看該作者
Modeling of Depositional Growth of Ice Crystal, independent from the size of ice crystal. Recently, a linear relation between the number and mass of ice crystal in the small range of ice crystal radius is assumed to develop new schemes. Four schemes are tested in a series of sensitivity experiments of pre-summer torrential rainfall event. In thi
54#
發(fā)表于 2025-3-31 00:16:45 | 只看該作者
Future Perspective of Cloud-Resolving Modeling,g TOGA COARE. The basic concept of cloud-resolving convection parameterization and its application to general circulation model simulations are discussed. Finally, cloud-resolving model is applied to the global domain for the improvement of precipitation simulations at global scale.
55#
發(fā)表于 2025-3-31 01:27:28 | 只看該作者
56#
發(fā)表于 2025-3-31 06:05:19 | 只看該作者
57#
發(fā)表于 2025-3-31 09:52:10 | 只看該作者
Anna Schnitzer,Andrea Bossen,Tanya Tyagunovag TOGA COARE. The basic concept of cloud-resolving convection parameterization and its application to general circulation model simulations are discussed. Finally, cloud-resolving model is applied to the global domain for the improvement of precipitation simulations at global scale.
58#
發(fā)表于 2025-3-31 13:58:35 | 只看該作者
59#
發(fā)表于 2025-3-31 18:06:01 | 只看該作者
Springer Atmospheric Scienceshttp://image.papertrans.cn/c/image/228506.jpg
60#
發(fā)表于 2025-4-1 01:09:23 | 只看該作者
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.
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