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Chin. Phys. B, 2011, Vol. 20(10): 109201    DOI: 10.1088/1674-1056/20/10/109201
GEOPHYSICS, ASTRONOMY, AND ASTROPHYSICS Prev  

Thermal aspect of the diurnal variation of tropical convective and stratiform rainfall

Cui Xiao-Peng(崔晓鹏)a)† and Li Xiao-Fan(李小凡)b)
a Laboratory of Cloud-Precipitation Physics and Severe Storms (LACS), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; b NOAA/NESDIS/Office of Research and Applications, Camp Springs, Maryland, USA
Abstract  The diurnal variation of radiation plays a key role in determining the diurnal variations of tropical oceanic convective and stratiform rainfall, and the examination of such a relationship requires a direct link between the radiation term in a heat budget and the surface rain rate in a cloud budget. Thus, the thermally related surface rainfall budgets derived from the combination of cloud and heat budgets are analysed with two-dimensional equilibrium cloud-resolving model simulation data to study the effects of sea surface temperature (SST) and cloud radiative, and microphysical processes on the diurnal variations of convective and stratiform rainfall. The results show that the increase in SST, the inclusion of diurnal variation of SST and the exclusion of cloud radiative processes increase negative diurnal anomalies of heat divergence over rainfall-free regions during the nighttime through changing the vertical structures of diurnal anomaly of radiation in the troposphere. The strengthened negative diurnal anomalies of heat divergence over rainfall-free regions enhance positive diurnal anomalies of heat divergence over convective regions, which intensifies the positive diurnal anomaly of convective rainfall. The exclusion of microphysical effects of ice clouds increases the negative diurnal anomaly of heat divergence over rainfall-free regions during the nighttime through reducing latent heat; this appears to enhance the positive diurnal anomaly of heat divergence over raining stratiform regions, and thus stratiform rainfall.
Keywords:  thermal aspects      diurnal variation      tropical convective and stratiform rainfall  
Received:  20 December 2010      Revised:  19 April 2011      Accepted manuscript online: 
PACS:  92.60.Ox (Tropical meteorology)  
  92.40.Ea (Precipitation)  
  92.05Fg  
  92.60.Nv (Cloud physics and chemistry)  
Fund: Project supported by the National Basic Research Program of China (Grant No. 2009CB421505), the Funds for International Cooperation and Exchange of the National Natural Science Foundation of China (Grant No. 40921160379), and the National Natural Science Foundation of China (Grant No. 40775036).

Cite this article: 

Cui Xiao-Peng(崔晓鹏) and Li Xiao-Fan(李小凡) Thermal aspect of the diurnal variation of tropical convective and stratiform rainfall 2011 Chin. Phys. B 20 109201

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