摘要
本文计算了平流层、中间层和低热层大气中各种光化过程的加热率与大气的冷却率，并且给出了20—140km的大气净加热率的昼夜变化特征．为大气潮汐波的研究提供了基础．
In this paper, the heating rate produced by photochemical processes in stratosphere,mesosphere and lower thermosphere is calculated. And the atmospheric cooling rate is calculated as well using Fondchev's code. Using one dimensional tine dependent photochemical model, the diurnal variation of heating rate in the height region of 20140 km is studied. Tis work provides theoretical basis for studying the atmospheric tidal waves.
出处
《空间科学学报》
CAS
CSCD
北大核心
1998年第2期146-151,共6页
Chinese Journal of Space Science
基金
国家自然科学基金!49574236
