2) lower stratospheric temperature
低平流层温度
3) troposphere average temperature
对流层平均温度
4) Smoothing temperature
流平温度
5) Temperature advection
温度平流
1.
A gale process accompanied by severe cold air in offshore of Jiangsu Province was analyzed in this paper and the relationships of wind field with evolution characteristics of surface allobaric field and allobaric field and its gradient that were increased by the cold temperature advection resulted in the gale offshore of Jiangsu.
对一次强冷空气伴随的近海大风天气进行了分析,研究了强冷空气影响过程中地面变压场和高空各层温度平流场的演变特征及其与地面风场之间的关系,在此基础上对强冷空气引发江苏近海强风形成与发展的物理过程进行了探讨,研究表明:温度平流与地面风场之间是通过变压场相互关联和促进的,强冷空气所伴随的冷平流增强了地面变压场及变压梯度,是导致江苏近海大风出现的重要原因。
2.
By analyzing the data of wind profile radar, we can calculate the size of the temperature advection, which can be used as an important indicator in short-time weather forecasts.
通过风廓线雷达数据计算垂直方向温度平流发现,在对流发展时,温度平流垂直廓线有明显的变化,对雷暴大风等强对流天气的预报有一定参考意义。
6) thermal advection
温度平流
1.
The results show that the intense thermal advection, vorticity advection, and latent heat release are the main factors contributing to the explosive development of cyclones.
认为强的温度平流、涡度平流、位涡平流和凝结潜热释放是使气旋爆发性发展的主要因子,爆发性气旋发展过程是一特殊的斜压过程,存在着某种自我激发的机制。
补充资料：铂电阻温度表(见电阻温度表)
铂电阻温度表(见电阻温度表)
表。bod旧nZu wendubiao铂电阻温度表见电阻温
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条