Atmospheric Thermodynamics and Vertical Stability
International Journal of Science and Research (IJSR)

International Journal of Science and Research (IJSR)
Call for Papers | Fully Refereed | Open Access | Double Blind Peer Reviewed

ISSN: 2319-7064


Downloads: 105 | Views: 415

Research Paper | Aerospace Engineering | Sudan | Volume 5 Issue 8, August 2016 | Popularity: 6.1 / 10


     

Atmospheric Thermodynamics and Vertical Stability

Mohamed Habib Ahmed ElKanzi


Abstract: There are three main types of processes in which be interested 1) Cooling or warming at constant pressure.2) Expansion or compression.3) Mixing. Vertical motion of air masses in the atmosphere are accompanied by changes in pressure. So there are adiabatic expansion with and without condensation condensation. when a region of the atmosphere is unstable, convection may ensue, with vertical ascents and compensating descents of air i. e vertical mixing as well as horizontal mixing so far, air can be forced to rise even in a stable atmosphere, so can be vertical stability, conditional and latent instability, potential or convective instability if the opposite happen, i. e that the humidity increases with height, the layer will become stable with lifting. it is the case of potential or convective stability.


Keywords: Thermodynamics Atmosphere Adiabatic expansion Mixing stability


Edition: Volume 5 Issue 8, August 2016


Pages: 1097 - 1102



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Mohamed Habib Ahmed ElKanzi, "Atmospheric Thermodynamics and Vertical Stability", International Journal of Science and Research (IJSR), Volume 5 Issue 8, August 2016, pp. 1097-1102, https://www.ijsr.net/getabstract.php?paperid=ART2016952, DOI: https://www.doi.org/10.21275/ART2016952

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