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The Improved Two-Dimensional Artificial Neural Network- Based Ionospheric Model (ANNIM)

机译:改进的二维人工神经基于网络的电离层模型(ANNIM)

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An artificial neural network-based two-dimensional ionospheric model (ANNIM) that can predict the ionospheric F2-layer peak density (NmF2) and altitude (hmF2) had recently been developed using long-term data of Formosat-3/COSMIC GPS radio occultation (RO) observations (Sai Gowtam & Tulasi Ram, 2017a, https://doi.org/10.1002/2017JA024795). In this current paper, we present an improved version of ANNIM that was developed by assimilating additional ionospheric data from CHAMP, GRACE RO, worldwide ground-based Digisonde observations, and by using a modified spatial gridding approach based on the magnetic dip latitudes. The improved ANNIM better reproduces the spatial and temporal variations of NmF2 and hmF2, including the postsunset enhancement in equatorial hmF2 associated with the prereversal enhancement in the zonal electric field. The ANNIM-predicted NmF2 and hmF2 exhibit excellent correlations with ground-based Digisonde observations over different solar activity periods. The ANNIM simulations under enhanced geomagnetic activity predict the depletion of NmF2 at auroral-high latitudes, and enhancement over low latitude to midlatitude with respect to quiet conditions, which is consistent with the storm time meridional wind circulation and the associated neutral composition changes. The improved ANNIM also predicts a significant enhancement in hmF2 around auroral latitudes due to increased plasma scale height associated with particle and Joule heating during storm periods. Further, the ANNIM successfully reproduces the coherent oscillations in NmF2 and hmF2 with recurrent cororating interaction region-driven geomagnetic activity during the extreme solar minimum year 2008 and can distinguish the roles of recurrent geomagnetic activity and solar irradiance through controlled simulations.
机译:一个人工神经网络二维的电离层模型(ANNIM)可以预测电离层F2-layer密度(NmF2)和峰值高度(hmF2)最近被开发使用长期数据Formosat-3 /宇宙GPS无线电隐藏(RO)的评论(Sai Gowtam &Tulasi内存,2017,https://doi.org/10.1002/2017JA024795)。现在的论文,我们提出一个改进的版本ANNIM由同化额外的电离层数据从冠军,优雅罗,全球地面Digisonde观察,通过使用修改后的空间网格的方法基于磁纬度。ANNIM更好的繁殖空间和时间NmF2和hmF2变化,包括在赤道hmF2 postsunset增强与prereversal增强有关纬向电场。NmF2和hmF2表现出良好的相关性地面Digisonde观察在不同的太阳活动周期。模拟在增强的地磁活动在auroral-high预测NmF2的损耗纬度,增强在纬度较低中间纬度对安静的条件下,这是符合风暴的时间吗经向风环流和相关中性成分变化。还预测在hmF2显著增强由于增加了等离子体在极光纬度规模高度相关的粒子和焦耳加热风暴时期。成功地再现了相干振荡在NmF2 hmF2 cororating复发交互region-driven地磁活动在太阳能最低2008年和极端能区分复发的角色吗地磁活动和太阳辐照度模拟控制。

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