Characteristics of cloud drop spectra in tropical warm clouds

1985 ◽  
Vol 123 (6) ◽  
pp. 930-940 ◽  
Author(s):  
S. K. Paul ◽  
A. G. Pillai ◽  
A. M. Selvam ◽  
A. S. R. Murty
MAUSAM ◽  
2021 ◽  
Vol 43 (4) ◽  
pp. 415-420
Author(s):  
S. K. PAUL ◽  
A. G . PILLAI

Measurements o f clo ud drop ..ire spectra on non-preci pitating cumulus clouds, 1·2 km thick,were made at differe nt levels o ver the Arabian Sea (maritime) and over r une (inland) regio n during the end ofthe summer monsoo n seasons of 1973, 1974 and 1979.The macimurn size of clo ud drops for the. Arabian Sea generally increased with height. while that for run eJiJ not show a systematic change with height. At bot h the local ions. the total concentration o f drops decreasedwith height. The maritime dist ributions were bimodal at all levels while those o..-er Punc were usually unimodal.The average values of liquid water content. mean vo lume diameter. dispersion and conccnt rarion of drops withdiameter > 50 «m were a lin le greater and total concentration a little smaller over the maritime region as ' om'pared to those over inland. The co ncentrations of drops with diameter < 14 ,...m and those > 78 I'm and thema ximum ~ i 7e were greater over Pune than o..er the sea. The ..'a riarions in cloud drop spectra and the clo udphysical parameters over beth the locations are discussed.Kc) words - Cloud drop size spectra, Drop co ncentration,


1981 ◽  
Vol 8 (3) ◽  
pp. 221-224 ◽  
Author(s):  
R. F. Pueschel ◽  
E. W. Barrett ◽  
D. L. Wellman ◽  
J. A. McGuire

2004 ◽  
Vol 109 (D13) ◽  
pp. n/a-n/a ◽  
Author(s):  
W. C. Conant ◽  
T. M. VanReken ◽  
T. A. Rissman ◽  
V. Varutbangkul ◽  
H. H. Jonsson ◽  
...  
Keyword(s):  

1949 ◽  
Vol 2 (3) ◽  
pp. 376 ◽  
Author(s):  
EB Kraus ◽  
B Smith

A theoretical study indicates that the number and size of the drops formed in a cloud vary with the rate of cooling, the initial temperature, and the air pressure. The faster the cooling rate, the lower the initial temperature, and the lower the altitude, the greater is the number of drops and the smaller their size. The drop size spectrum also depends, to a large extent, on the number of available condensation nuclei. Furthermore, it tends to be widened by sedimentation and turbulence.


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