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Empirical model of global thermospheric temperature and composition based on data from the OGO-6 quadrupole mass spectrometer

机译:基于OGO-6四极质谱仪数据的全球热层温度和成分的经验模型

摘要

An empirical global model for magnetically quiet conditions has been derived from longitudinally averaged N2, O, and He densities by means of an expansion in spherical harmonics. The data were obtained by the OGO-6 neutral mass spectrometer and cover the altitude range 400 to 600 km for the period 27 June 1969 to 13 May 1971. The accuracy of the analytical description is of the order of the experimental error for He and O and about three times experimental error for N2, thus providing a reasonable overall representation of the satellite observations. Two model schemes are used: one representing densities extrapolated to 450 km and one representing densities extrapolated to 120 km with exospheric temperatures inferred from N2 densities. Using the best fit model parameters the global thermospheric structure is presented in the form of a number of contour plots.
机译:通过球谐函数的扩展,从纵向平均的N2,O和He密度中得出了一个磁静条件的经验全局模型。数据是通过OGO-6中性质谱仪获得的,涵盖了1969年6月27日至1971年5月13日期间400至600 km的海拔范围。分析描述的准确性约为He和O的实验误差的量级。和N2的大约三倍的实验误差,从而提供了卫星观测的合理总体表示。使用了两种模型方案:一种代表根据N2密度推断出的大气层温度外推至450 km的密度,另一种代表根据外推温度推断至120 km的密度。使用最佳拟合模型参数,以许多等高线图的形式显示了整体热球结构。

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