摘要
通过一个思想实验把大气密度的时空分布函数与一个概率分布函数联系了起来，又利用最大熵原理导出了一个新的全球大气的方程，即大气密度方程。文章给出了它的通解并指出等温大气的压力高度公式是它的一个特解。对这个新的理论思路，新的方程和它的应用潜力作了初步讨论。
fter an idea experiment, it is proved that the spatial and temporal distribution function of the globe atmosphere is in direct proportion to a probability density distribution function. Using the relationship between probability and maximum entropy principle, a new equation for global atmosphere is reduced that is atmospheric density equation. Its general resolution has heen gotten and the pressure height formula is a special solution of this equation. Some concerning problems are also discussed in this paper.
出处
《气象学报》
CSCD
北大核心
1998年第3期377-382,共6页
Acta Meteorologica Sinica
