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平流层,中间层,低热层大气加热过程特性研究
Alternative TitleTHE STUDY OF TIC HEATING PROCESSES IN STRATOSPHERE,MESOSPHERE AND LOWER THERMOSPHERE
徐寄遥; 王英鉴; 北京8701信箱
Department空间天气学国家重点实验室
Source Publication空间科学学报
1998
Volume18Issue:2Pages:146-151
ISSN0254-6124
Language中文
Keyword加热率 冷却率 大气 平流层 中间层 低热层
Abstract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.
Other Abstractin this paper,the heating rate produced by otochemical processes in stratosphere,mesosphere and lower thermosphere is calculated. And the atmospheric cooling rate is calculated as well using Fornichev's code.Using one dimensional time dependent-otochemical model,the diurnal variation of heating rate in the height region of 20-l40km is studied,This work provides theoretical basis for studying the atmospheric tidal waves.
Indexed ByCSCD
Funding Project中国科学院空间科学与应用研究中心
Citation statistics
Document Type期刊论文
Identifierhttp://ir.nssc.ac.cn/handle/122/1410
Collection空间科学部
Corresponding Author北京8701信箱
Recommended Citation
GB/T 7714
徐寄遥,王英鉴,北京8701信箱. 平流层,中间层,低热层大气加热过程特性研究[J]. 空间科学学报,1998,18(2):146-151.
APA 徐寄遥,王英鉴,&北京8701信箱.(1998).平流层,中间层,低热层大气加热过程特性研究.空间科学学报,18(2),146-151.
MLA 徐寄遥,et al."平流层,中间层,低热层大气加热过程特性研究".空间科学学报 18.2(1998):146-151.
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