基于GPS層析反演和斜向返回探測反演的電離層二維電子密度重構(gòu)
doi: 10.11999/JEIT150981
基金項(xiàng)目:
國家自然科學(xué)基金(41204111, 41574146)
Two Dimensional Ionospheric Electron Density Reconstruction Based on GPS Tomography and Oblique Backscatter Inversion
Funds:
The National Natural Science Foundation of China (41204111, 41574146)
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摘要: GPS層析反演和電離層斜向返回探測反演可以給出電離層大尺度2維電子濃度分布,該文基于3次電離層垂測、GPS層析探測和斜向返回探測的實(shí)驗(yàn)結(jié)果,比較了GPS層析反演和電離層斜向返回探測反演得到的大尺度電子密度2維分布。結(jié)果表明GPS層析和電離層斜向返回探測都能較好地重構(gòu)電離層電子密度分布,反映電離層大尺度的空間結(jié)構(gòu)。通過和電離層垂測結(jié)果的比較,表明GPS層析和斜向返回探測反演得到電離層F2層最大電子密度和峰高具有較好的精度。Abstract: Both GPS Computerized Ionosphere Tomography (CIT) and BackScatter Ionosonde (BSI) can provide two-dimensional electron density profile in large scale. Based on the result of three separate vertical ionosonde, GPS computerized ionosphere tomography and backscatter ionosonde, this paper compares the two-dimensional electron density profiles of GPS computerized ionosphere tomography and backscatter ionosonde. The results show that both methods reconstruct two-dimensional electron density profiles very well and reflect spatial structure of ionosphere. These two methods show high accuracy in the biggest electron density and peak height of F2 layer in contrast with the result of Vertical Ionosonde (VI).
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