Effects of cloud microphysics on monsoon convective system and its formation environments over the South China Sea: A two-dimensional cloud-resolving modeling study

2011 ◽  
Vol 116 (D7) ◽  
Author(s):  
Danhong Fu ◽  
Xueliang Guo ◽  
Changhai Liu
2020 ◽  
Vol 186 ◽  
pp. 102367
Author(s):  
Chuanjun Du ◽  
Jianping Gan ◽  
Chiwing Rex Hui ◽  
Zhongming Lu ◽  
Xiaozheng Zhao ◽  
...  

2007 ◽  
Vol 64 (2) ◽  
pp. 360-380 ◽  
Author(s):  
Jian-Jian Wang ◽  
Xiaofan Li ◽  
Lawrence D. Carey

Abstract A two-dimensional cloud-resolving simulation is combined with dual-Doppler and polarimetric radar analysis to study the evolution, dynamic structure, cloud microphysics, and rainfall processes of monsoon convection observed during the South China Sea (SCS) summer monsoon onset. Overall, the model simulations show many similarities to the radar observations. The rainband associated with the convection remains at a very stable position throughout its life cycle in the northern SCS. The reflectivity pattern exhibits a straight upward structure with little tilt. The positions of the convective, transition, and stratiform regions produced by the model are consistent with the observations. The major difference from the observations is that the model tends to overestimate the magnitude of updraft. As a result, the maximum reflectivity generated by the model appears at an elevated altitude. The surface rainfall processes and associated thermodynamic, dynamic, and cloud microphysical processes are examined by the model in terms of surface rainfall, temperature and moisture perturbations, circulations, and cloud microphysical budget. At the preformation and dissipating stages, although local vapor change and vapor convergence terms are the major contributors in determining rain rate, they cancel each other out and cause little rain. The vapor convergence/divergence is closely related to the lower-tropospheric updraft/subsidence during the early/late stages of the convection. During the formation and mature phases, vapor convergence term is in control of the rainfall processes. Meanwhile, water microphysical processes are dominant in these stages. The active vapor condensation process causes a large amount of raindrops through the collection of cloud water by raindrops. Ice microphysical processes including riming are negligible up to the mature phase but are dominant during the weakening stage. Cloud source/sink terms make some contributions to the rain rate at the formation and weakening stages, while the role of surface evaporation term is negligible throughout the life cycle of the convection.


2002 ◽  
Vol 55 (3) ◽  
pp. 225 ◽  
Author(s):  
Y. Lin ◽  
J. Wang ◽  
X. Wu ◽  
S. Zhou ◽  
L. L. P. Vrijmoed ◽  
...  

A novel cyclic depsipeptide, enniatin G, together with enniatins B and B4 were isolated from the mangrove fungus Halosarpheia sp.(strain 732) from the South China Sea. Their structures were determined by analysis of spectroscopic data, mainly two-dimensional nuclear magnetic resonance experiments. Enniatin G exhibited activity against Heps 7402, ED50 12mg/mL.


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