| 一氧化氮冷却率的变化及其作用 |
| |
| 引用本文： | 徐秀娟.一氧化氮冷却率的变化及其作用[J].空间科学学报,1996,16(3):240-244. |
| |
| 作者姓名： | 徐秀娟 |
| |
| 作者单位： | 中国科学院空间科学与应用研究中心, 北京100080 |
| |
| 摘 要： | 利用最新的NO经验公式,计算了近两个太阳活动周期100-200km间NO的冷却率,研究了太阳和地磁活动对NO和O冷却率的影响。进一步证明了NO冷却是120km以上热层的主要冷却过程。
|
| 关 键 词： | NO 大气发射 |
| 收稿时间： | 1994-12-23 |
VARIATIONS NITRIC OXIDE COOLING RATE AND ITS EFFECT |
| |
| xu kin-juan.VARIATIONS NITRIC OXIDE COOLING RATE AND ITS EFFECT[J].Chinese Journal of Space Science,1996,16(3):240-244. |
| |
| Authors: | xu kin-juan |
| |
| Institution: | Ceater for Space Science and Applied Research, Academia Sinica, Beijing 100080 |
| |
| Abstract: | The cooling rate of Nitric Oxide is calculated by using recently developed empirical formula of Nitric Oxide density.The effeCt of solar and.geomagnetic activity on Nitric Oxide cooling rate is studied.The main results obtained are:(1)the cooling rate and the height of maximum cooling rate occurrence periedicly varies with solar activity;(2) the variation rule with solar zenith angle are not symmetry.before and after noon;(3) it is found that the cooling rate of Nitric Oxide is not only larger than Oxigen atoms,but also its response to solar and geomagnetic activity is far more sensitive than Oxigen atoms. It is proved that Nitric Oxide cooling is a major cooling process above 120Km in the thermosphere. |
| |
| Keywords: | Nitric Oxide Atmospheric emission |
| 本文献已被 CNKI 维普 等数据库收录！ |
| 点击此处可从《空间科学学报》浏览原始摘要信息 |
| 点击此处可从《空间科学学报》下载免费的PDF全文 |
