Advanced Fluid Dynamics 2012
DOI: 10.5772/26535
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Influence of Horizontal Temperature Gradients on Convective Instabilities with Geophysical Interest

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“…Due to the fierce upward motion generally a downward motion is developing in the middle of the whirls. According to in situ and model measurements as well as simulations the core of the whirls is warmer than its environment (Emmons and Ying, 1967;Zhao et al, 2004;Balme and Greeley, 2006;Herrero et al, 2012). The descending air is moving nearly adiabatically therefore it becomes warmer than the air in the wall of the whirl where the air is moving upwards (also nearly adiabatically).…”
Section: Scientific Backgroundmentioning
confidence: 99%
“…Due to the fierce upward motion generally a downward motion is developing in the middle of the whirls. According to in situ and model measurements as well as simulations the core of the whirls is warmer than its environment (Emmons and Ying, 1967;Zhao et al, 2004;Balme and Greeley, 2006;Herrero et al, 2012). The descending air is moving nearly adiabatically therefore it becomes warmer than the air in the wall of the whirl where the air is moving upwards (also nearly adiabatically).…”
Section: Scientific Backgroundmentioning
confidence: 99%