Estudio del Fenómeno de Mezcla de Nubes con un Simple Modelo Numérico 3D
Abstract
In this paper the study of the entrainment in cloud is presented using the wind, temperature, pressure, and water contents fields of a 3D numerical cloud model.
This study is done using two parameters that conserved with adiabatic altitude changes and that mix in a nearly manner. they are the total water contents and the equivalent potential temperature.
The results show that the conclusions obtain with "in situ" measurement are recuperated.
Also can be concluded that the entrainment with upper sector will be turbulent and not organizated. For other hand this results confirm the good performance of the numerical cloud model. The advantage of numerical estudy of cloud physics are showed.
This study is done using two parameters that conserved with adiabatic altitude changes and that mix in a nearly manner. they are the total water contents and the equivalent potential temperature.
The results show that the conclusions obtain with "in situ" measurement are recuperated.
Also can be concluded that the entrainment with upper sector will be turbulent and not organizated. For other hand this results confirm the good performance of the numerical cloud model. The advantage of numerical estudy of cloud physics are showed.
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