An intense rainbow at the base of a large Towering Cumulus cloud

Weather ◽  
2022 ◽  
Vol 77 (1) ◽  
Keyword(s):  
Cumulus Cloud

Size Statistics of Cumulus Cloud Populations in Large-Eddy Simulations

2003 ◽  
Vol 60 (8) ◽  
pp. 1060-1074 ◽  
Author(s):  
R. A. J. Neggers ◽  
H. J. J. Jonker ◽  
A. P. Siebesma
Keyword(s):  
Large Eddy Simulations ◽  
Cumulus Cloud ◽  
Large Eddy

On the size dependence of cumulus cloud spacing

2021 ◽  
Author(s):  
Thirza van Laar ◽  
Roel A J Neggers
Keyword(s):  
Size Dependence ◽  
Cumulus Cloud

A Measurement of the Velocity Field of a Cumulus Cloud

1973 ◽  
Vol 12 (5) ◽  
pp. 841-846 ◽  
Author(s):  
J. Levine ◽  
M. Garstang ◽  
N. E. LaSeur
Keyword(s):  
Velocity Field ◽  
Cumulus Cloud

scholarly journals The Formation of Cumulus Cloud above Bush-fires

Nature ◽  
1924 ◽  
Vol 113 (2830) ◽  
pp. 126-126
Author(s):  
W. G. DUFFIELD
Keyword(s):  
Cumulus Cloud

Study of Thermal Activity in The Mixing Layer During First Generated Single Cloud by Using Combined Observation From Boundary Layer Radar, Doppler Lidar and Time Lapse Camera 

2021 ◽  
Author(s):  
Ginaldi Ari Nugroho ◽  
Kosei Yamaguchi ◽  
Eiichi Nakakita ◽  
Masayuki K. Yamamoto ◽  
Seiji Kawamura ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Time Series ◽  
Atmospheric Boundary Layer ◽  
Vertical Velocity ◽  
Time Lapse ◽  
Small Scale ◽  
Thermal Activity ◽  
Doppler Lidar ◽  
Cumulus Cloud ◽  
Scale Perturbation

<p>Detailed observation of small scale perturbation in the atmospheric boundary layer during the first generated cumulus cloud are conducted. Our target is to study this small scale perturbation, especially related to the thermal activity at the first generated cumulus cloud. The observation is performed during the daytime on August 17, 2018, and September 03, 2018. Location is focused in the urban area of Kobe, Japan. High-resolution instruments such as Boundary Layer Radar, Doppler Lidar, and Time Lapse camera are used in this observation. Boundary Layer Radar, and Doppler Lidar are used for clear air observation. Meanwhile Time Lapse Camera are used for cloud existence observation. The atmospheric boundary layer structure is analyzed based on vertical velocity profile, variance, skewness, and estimated atmospheric boundary layer height. Wavelet are used to observe more of the period of the thermal activity. Furthermore, time correlation between vertical velocity time series from height 0.3 to 2 km and image pixel of generated cloud time series are also discussed in this study.</p>

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