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WEEK 35 2011
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Oxnard
Weather
Underground |
Lancaster Weather
Underground |
Martinez
WeatherUnderground |
The thermodynamic structure of the hurricane can be modelled as a heat engine [3] running between sea temperature of about 300K and tropopause which has temperature of about 200K. Parcels of air traveling close to the surface take up moisture and warm, ascending air expands and cools releasing moisture (rain) during the condensation. The release of latent heat energy during the condensation provides mechanical energy for the hurricane. |