首页> 外文会议>Joint International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics >ESTIMATION OF CRITICAL FREQUENCY AND HEIGHT MAXIMUM FOR PATH' MIDDLE POINT ON EVIDENCE DERIVED FROM EXPERIMENTAL OBLIQUE SOUNDING DATA. COMPARISON OF CALCULATED VALUES WITH EXPERIMENTAL AND IRI VALUES
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ESTIMATION OF CRITICAL FREQUENCY AND HEIGHT MAXIMUM FOR PATH' MIDDLE POINT ON EVIDENCE DERIVED FROM EXPERIMENTAL OBLIQUE SOUNDING DATA. COMPARISON OF CALCULATED VALUES WITH EXPERIMENTAL AND IRI VALUES

机译:估计实验倾斜数据源自实验倾斜数据的临界频率和高度最大值。实验和IRI值计算值的比较

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The work is devoted to experimental checking of technique for estimation of f_0F2 and hmF2 values in path' midpoint through oblique sounding (OS) data. In this work data obtained by Irkutsk chirp-sounder on the Norilsk-Irkutsk path were used and data obtained by Podkamennaya Tunguska ionospheric station (which located near estimating path' middle point) were used also. During the calculation, the experimental distance-frequency characteristics (DFC) of path are recalculated into height-frequency characteristics (HFC) in path' midpoint by means of Smith method. It lets us to determine f_0F2 value in path' middle point. For hmF2 definition N(h) profile is used which was obtained by recalculation of HFC by means the Guliaeva technique. Also the fast method of recalculation was probed in two DFC points. In the work comparison was made between calculated f_0F2 values and experimental f_0F2 values obtained by Podkamennaya Tunguska ionospheric station. Comparison of estimating hmF2 values with values calculated by Dudeney method from experimental f_0E, f_0F2, M(3000)F2 values at Podkamennaya Tunguska was carried out. In addition, estimating values was compared with values given by the IRI model. A capability of the IRI model adaptation by f_0F2 and hmF2 values was investigated. It will help during diagnostics, working out regional models of ionosphere and during the adaptation of various models of ionosphere to the real conditions.
机译:该工作致力于通过倾斜探测(OS)数据在路径中估算路径中的F_0F2和HMF2值估计技术。在使用Norilsk-Irkutsk路径上的Irkutsk Chirp-Loute获得的工作数据,也使用了由Podkamennaya Tunguska电离层(位于估计路径'中间点附近)获得的数据。在计算过程中,通过史密斯方法将路径的实验距离 - 频率特性(DFC)重新计算到路径中的高度频率特性(HFC)中。它可以让我们确定路径中的中间点中的f_0f2值。对于HMF2定义,使用N(h)曲线,通过通过Guliaeva技术重新计算HFC而获得的。此外,在两个DFC点中探测了快速重新计算的方法。在工作比较中,在计算出的F_0F2值和由Podkamennaya Tunguska电离层所获得的实验F_0F2值之间进行。通过从实验F_0e,Podkamennaya tunguska的实验F_0e,f_0f2,m(3000)F2值的Dudeney方法计算HMF2值的比较。另外,将估计值与IRI模型给出的值进行比较。研究了F_0F2和HMF2值的IRI模型适应的能力。它将在诊断过程中有所帮助,锻炼电离层的区域模型和在各种模型的电离层适应真实条件下。

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