Thermodynamic Processes in the Moist Atmosphere
Thermodynamic Processes in the Moist Atmosphere
复制标题
潮湿大气中的热力学过程
DOI：
10.2113/gselements.6.5.293
复制
发表时间：
2010
期刊：
影响因子：
4.5
通讯作者：
A. Bott
中科院分区：
文献类型：
--
作者：
A. Bott
热力学原理在地球大气中发生的几乎所有过程中都起着关键作用。它们在大气层的热分层、各种区域性和大规模风系统的出现以及云和降水的形成中表现得非常明显。重要的是要注意，简化热力学的应用通常足以描述大尺度大气过程。然而，为了深入了解云的微物理结构，需要对复杂的热力学云过程进行详细的研究。
Thermodynamic principles play a key role in almost all processes occurring in the Earth9s atmosphere. They are formidably expressed in the thermal stratification of the atmosphere, in the appearance of various regional and large-scale wind systems, as well as in the formation of clouds and precipitation. It is important to note that the application of simplified thermodynamics is usually sufficient to describe large-scale atmospheric processes. However, for an in-depth understanding of the microphysical structure of clouds, a detailed investigation of the complex thermodynamic cloud processes is needed.