摘要
在对流层内,运用理想气体绝热过程的理想模型,从理论上定性分析了大气温度随高度升高而下降的原因,定量推导了其变化率,并把结果与实际测量值进行了比较分析。
By using the ideal gas model in the adiabatic process, this paper analyses qualitatively the reasons for the dropping of atmospheric temperature with the increasing of height in the troposphere and verify the rate of change quantitatively. Then the calculated results are compared with the actual numbers.
出处
《河南科技学院学报》
2007年第2期32-32,45,共2页
Journal of Henan Institute of Science and Technology(Natural Science Edition)
关键词
大气
对流层
温度
变化率
绝热过程
atmosphere
troposphere
temperature
rate of change
adiabatic process
