|Accueil > UNIVERSITE FELIX HOUPHOUET-BOIGNY > Articles UFHB > LINEAR STABILITY INVESTIGATION OF AN ACTIVE ATMOSPHERIC WARM CLOUD FLOW|
In this paper, the linear stability of an active cloud is investigated.
A Jean scale of about 8.75 km thick is revealed in which small cumuli can grow up within a vertically 2.5 km large band.
The study revealed that internal waves are stable and exhibit an acoustic behavior while the mechanism sustaining the flow instability is found
to be gravity-driven. The further analysis revealed that at the first stage, the entrainment process is required for the cloud to be fed in water
vapor until the droplets can grow by self-conversion, collision, accretion, coalescence and overcome the updraft winds. From this stage,
the gravity effects become the dominant instability mechanism that drives the cloud dynamics from a passive to an active behavior.
Keyword(s): stability ; dispersion relation ; cloud ; cumulus ; mixing ratio
The record appears in these collections:
UNIVERSITE FELIX HOUPHOUET-BOIGNY > Articles UFHB
Bibliothèque Virtuelle de l'Enseignement Supérieur et de la Recherche Scientifique