On the distribution and continuity of water substance in atmospheric circulations
On the distribution and continuity of water substance in atmospheric circulations
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DOI：
10.1007/978-1-935704-36-2_1
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发表时间：
1969
期刊：
影响因子：
--
通讯作者：
E. Kessler
中科院分区：
文献类型：
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作者：
E. Kessler
在连续性原理、模式气流和微物理过程模式的框架内考虑大气环流中水分的保存和分布。对降水的最简单的考虑包括它在上升气流柱中的垂直分布，在那里凝结物立即出现为具有均匀终端下降速度的降水。这项研究还处理稳定的二维空气环流，其中随时间变化的水蒸气，云和降水的分布模式microphysical processes.The方法在整个基本上是运动学，虽然结果提供了许多见解的动力学性质的多云或暴风雨的气氛。水的分布解释与空气的水平发散，垂直速度和压缩性，并经常提出物理图片。研究结果与降水天气系统的各种观测结果进行了比较。本文的详细摘要按章节在第1节和第15节中介绍。
The conservation and distribution of water substance in atmospheric circulations is considered within a frame of continuity principles, model air flows, and models of microphysical processes. The simplest considerations of precipitation involve its vertical distribution in an updraft column, where condensate appears immediately as precipitation with uniform terminal fallspeed. The study also treats steady two-dimensional air circulations in which time-dependent distributions of water vapor, cloud and precipitation respond to model microphysical processes.The approach throughout is essentially kinematic, although results provide numerous insights into the dynamical properties of a cloudy or stormy atmosphere. Water distributions are explained in relation to the air’s horizontal divergence, vertical velocity and compressibility, and physical pictures are presented frequently. The findings are compared with various observations on precipitating weather systems.Detailed summaries of this paper by Sections are presented in Sections 1 and 15.