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1)  warm layer of inversion
逆温暖层
1.
Also the causes of inversion occurrence and the agroclimatic ecological superiority of the warm layer of inversion which adapts to the biological characteristics of citrus trees are expounded.
本文探讨了陇南白龙江流域河谷浅山区冬季温度分布及逆温出现的特点;阐述了逆温形成的原因及与桔树生物学特性相适应的“逆温暖层”农业气候、生态的优势;根据冬季宏观温度和山体逆温分布规律,提出了浅山“暖层”宜桔地选择的方法。
2)  warm temperature stratification
暖温层积
3)  Inversion layer
逆温层
1.
Relationship between black body temperature and water vapour,precipitation and inversion layer;
水汽、降水和逆温层与卫星红外测值的关系分析
2.
The other important reason is that inversion layer were lifted from the ground to lower level of the air and maintained.
由于地面升温,逆温层从地面抬升至低空并稳定维持,是平流雾形成后能维持较久的又一重要原因。
4)  temperature inversion
逆温层
1.
The article analyses the influence factors such as the formation of the temperature inversion and the features of the causes of the pollution, so as to put forward to feasible methods and resolving channels aiming a.
乌鲁木齐所处山谷地形、三面环山的特殊地理条件所形成的逆温层是造成大气严重污染的主要原因。
2.
The turbulent characteristics in convective boundary layer topped temperature inversion were numerically investigated in terms of large eddy simulation.
采用大涡模拟方法研究了存在逆温层的情况下大气对流边界层的湍流特性。
3.
Results suggest that temperature inversion plays an important role in the formation an.
结果表明:逆温层对雾的形成和维持起着重要的作用,而雾又对大气边界层中的温、湿、风结构产生重要影响。
5)  low-level inversion
低层逆温
1.
Based on the ground-level meteorological data and low-level sonde data from July to August,2000 in Nanjing,the characteristics of thickness and intensity of low-level inversion (LLINV) are discussed,especially on their relations to urban surface temperature and relative humidity variation as well as their influence on body discomfort status.
利用 2 0 0 0年夏季南京城区地面气象要素和低层探空资料 ,分析了该年夏季南京城区早、晚低层逆温的频率、厚度和强度变化特征 ,着重从统计角度定量研究了逆温的厚度、强度与城区地面温度、相对湿度变化的关系及对人体舒适状况的影响。
6)  Multi-inversion
多层逆温
补充资料:提婆五逆与三逆
【提婆五逆与三逆】
 (故事)(参见:五逆)
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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