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A Method of Inversing the Peak Density of Atomic Oxygen Vertical Distribution in the MLT Region From the OI (557.7nm) Night Airglow Intensity

H. Gao J.Y. Xu W. Yuan

H. Gao, J.Y. Xu, W. Yuan. A Method of Inversing the Peak Density of Atomic Oxygen Vertical Distribution in the MLT Region From the OI (557.7nm) Night Airglow Intensity[J]. 空间科学学报, 2005, 25(5): 484-489. doi: 10.11728/cjss2005.05.484
引用本文: H. Gao, J.Y. Xu, W. Yuan. A Method of Inversing the Peak Density of Atomic Oxygen Vertical Distribution in the MLT Region From the OI (557.7nm) Night Airglow Intensity[J]. 空间科学学报, 2005, 25(5): 484-489. doi: 10.11728/cjss2005.05.484
H. Gao, J.Y. Xu, W. Yuan. A Method of Inversing the Peak Density of Atomic Oxygen Vertical Distribution in the MLT Region From the OI (557.7nm) Night Airglow Intensity[J]. Journal of Space Science, 2005, 25(5): 484-489. doi: 10.11728/cjss2005.05.484
Citation: H. Gao, J.Y. Xu, W. Yuan. A Method of Inversing the Peak Density of Atomic Oxygen Vertical Distribution in the MLT Region From the OI (557.7nm) Night Airglow Intensity[J]. Journal of Space Science, 2005, 25(5): 484-489. doi: 10.11728/cjss2005.05.484

A Method of Inversing the Peak Density of Atomic Oxygen Vertical Distribution in the MLT Region From the OI (557.7nm) Night Airglow Intensity

doi: 10.11728/cjss2005.05.484

A Method of Inversing the Peak Density of Atomic Oxygen Vertical Distribution in the MLT Region From the OI (557.7nm) Night Airglow Intensity

  • 摘要: In this paper, using the MSISE-90 model as the reference atmosphere, we discuss the feasibility and method of deducing the peak densities of the undisturbed atomic oxygen profiles in the MLT region (the mesosphere and lower thermosphere region) from OI (557.7 nm) night airglow intersities. The peak densities for different seasons, latitudes and longitudes are deduced from OI (557.7nm) airglow intensities through this expression. We analyze the features of inversion relative errors and discuss the influence of the variations in temperature on inversion errors. The results indicate that all inversion errors are less than 5% except for those at high altitudes in the summer hemisphere. And the impact of the variations in temperature on errors is not significant.

     

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出版历程
  • 收稿日期:  1900-01-01
  • 修回日期:  1900-01-01
  • 刊出日期:  2005-09-15

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