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Nonequilibrium thermodynamics of circulation regimes in optically thin, dry atmospheres

机译:在光学稀薄,干燥的大气中,循环状态的非平衡热力学

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摘要

An extensive analysis of an optically thin, dry atmosphere at different values of the thermal Rossby number Ro and of the Taylor number F_f is performed with a general circulation model by varying the rotation rate Ω and the surface drag τ in a wide parametric range. By using nonequilibrium thermodynamics diagnostics such as material entropy production, efficiency, meridional heat transport and kinetic energy dissipation we characterize in a new way the different circulation regimes. Baroclinic circulations feature high mechanical dissipation, meridional heat transport, material entropy production and are fairly efficient in converting heat into mechanical work. The thermal dissipation associated with the sensible heat flux is found to depend mainly on the surface properties, almost independent from the rotation rate and very low for quasi-barotropic circulations and regimes approaching equatorial super-rotation. Slowly rotating, axisymmetric circulations have the highest meridional heat transport. At high rotation rates and intermediate-high drag, atmospheric circulations are zonostrophic with very low mechanical dissipation, meridional heat transport and efficiency. When τ is interpreted as a tunable parameter associated with the turbulent boundary layer transfer of momentum and sensible heat, our results confirm the possibility of using the Maximum Entropy Production Principle as a tuning guideline in the range of values of Ω. This study suggests the effectiveness of using fundamental nonequilibrium thermodynamics for investigating the properties of planetary atmospheres and extends our knowledge of the thermodynamics of the atmospheric circulation regimes.
机译:通过在宽的参数范围内改变转速Ω和表面阻力τ,使用普通的循环模型对光学稀薄的干燥大气进行了广泛的分析,其中所述热罗斯伯数Ro与泰勒数F_f不同。通过使用非平衡热力学诊断,例如材料熵的产生,效率,子午热传递和动能耗散,我们以新的方式表征了不同的循环方式。斜压循环具有较高的机械耗散,经向热传递,材料熵产生,并且在将热量转换为机械功方面相当有效。发现与显热通量相关的热耗散主要取决于表面性质,几乎与旋转速率无关,并且对于准正压环流和接近赤道超旋转的状态非常低。缓慢旋转的轴对称环流具有最高的子午热传递。在高转速和中高阻力下,大气环流是带地层营养的,具有极低的机械耗散,子午热传递和效率。当将τ解释为与动量和显热的湍流边界层传递相关的可调参数时,我们的结果证实了在Ω值范围内使用最大熵产生原理作为调整准则的可能性。这项研究表明,使用基本的非平衡热力学来研究行星大气的性质是有效的,并且扩展了我们对大气环流热力学知识的了解。

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