gregarious 发表于 2025-3-25 06:56:05
http://reply.papertrans.cn/24/2309/230830/230830_21.pngAGGER 发表于 2025-3-25 08:30:35
http://reply.papertrans.cn/24/2309/230830/230830_22.pngCondyle 发表于 2025-3-25 12:17:14
Book 2008ness Media B. V. 2008 Keywords Aeronomy The term “aeronomy” has been used widely for many decades, but its origin has mostly been lost over the years. It was introduced by Sydney Chapman in a Letter to the Editor, entitled “Some Thoughts on Nomenclature”, in Nature in 1946 (Chapman 1946). In that le删减 发表于 2025-3-25 16:33:41
1385-7525 blished in the journal Space Science Reviews, Volume 139, Nos 1–4. DOI: 10. 1007/s11214-008-9353-0 © Springer Science+Business Media B. V. 2008 Keywords Aeronomy The term “aeronomy” has been used widely for many decades, but its origin has mostly been lost over the years. It was introduced by Sydney小争吵 发表于 2025-3-25 21:23:26
http://reply.papertrans.cn/24/2309/230830/230830_25.png责问 发表于 2025-3-26 00:48:49
Neutral Upper Atmosphere and Ionosphere Modeling,ere numerical modeling tools, the equations solved and key assumptions made, specified inputs and tunable parameters, their common applications, and finally their notable strengths and weaknesses. Examples of these model classes and their specific applications to individual planetary environments will be described.accessory 发表于 2025-3-26 05:03:57
Andrew F. Nagy,André Balogh,Ingo Mueller-WodargCovers all aspects of solar system aeronomy.Presents the observations and findings of many recent space missions会犯错误 发表于 2025-3-26 10:12:53
http://reply.papertrans.cn/24/2309/230830/230830_28.png驾驶 发表于 2025-3-26 12:39:56
https://doi.org/10.1007/978-3-658-03010-0s that they produce may interact with thermospheric neutral species producing dissociation, ionization, excitation, and heating. The interaction of X-rays or keV electrons with atmospheric neutrals may produce core-ionized species, which may decay by the production of characteristic X-rays or Augerindecipherable 发表于 2025-3-26 19:29:51
https://doi.org/10.1007/978-3-658-03010-0environments. These tools are commonly used to predict upper atmosphere and ionosphere characteristics and to interpret measurements once they are obtained. Additional applications of these tools include conducting diagnostic balance studies, converting raw measurements into useful physical paramete