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Solar EUV flux, exospheric temperature and thermospheric wind inferred from incoherent scatter measurements of the electron density profile at Millstone Hill and Shigaraki - art. no. 1358

机译:从密尔斯顿山和Shigaraki的电子密度分布的非相干散射测量推导出太阳EUV通量,大气层温度和热层风-艺术。没有。 1358

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摘要

1] We explore a method for inferring solar EUV flux, atmospheric composition and wind using ionospheric electron density Ne profile measurements. Incoherent scatter radar data from Millstone Hill and Shigaraki measured on October 5, 1989 are assimilated into a theoretical model whose driving forces, solar EUV flux, exosphere temperature Tex, and meridional wind, are adjustable. Adjustments are made to give best match between the model Ne profile and the data. The derived Tex values, found to be low near noon at Millstone and high in the afternoon at Shigaraki, are essentially those required to give the [O]/[N-2] ratio necessary to fit the data. Our inferred EUV fluxes for the two sites are similar. Our technique of using profile data may resolve the ambiguity in deriving EUV and [O]/[N-2] from electron-density measurements. [References: 15
机译:1]我们探索了一种利用电离层电子密度Ne剖面测量来推断太阳EUV通量,大气成分和风的方法。 1989年10月5日测得的Millstone Hill和Shigaraki的非相干散射雷达数据被同化为理论模型,该模型的驱动力,太阳EUV通量,大气层温度Tex和子午风是可以调整的。进行调整以使模型Ne轮廓和数据之间达到最佳匹配。得出的Tex值,在密尔斯顿的正午时分较低,而在Shigaraki的下午时较高,基本上是给出拟合数据所需的[O] / [N-2]比所需的值。我们推断出的两个位置的EUV通量相似。我们使用轮廓数据的技术可以解决从电子密度测量得出EUV和[O] / [N-2]时的歧义。 [参考:15

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