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|    ScienceDaily to All    |
|    A more precise model of the Earth's iono    |
|    24 Apr 23 22:30:26    |
      MSGID: 1:317/3 64475775       PID: hpt/lnx 1.9.0-cur 2019-01-08       TID: hpt/lnx 1.9.0-cur 2019-01-08        A more precise model of the Earth's ionosphere         With the help of neural networks, the complexity of the layer around the       Earth can be reconstructed much better than before. This is important for       satellite navigation, among other things.                Date:        April 24, 2023        Source:        GFZ GeoForschungsZentrum Potsdam, Helmholtz Centre        Summary:        The ionosphere -- the region of geospace spanning from 60 to 1000        kilometers above the Earth -- impairs the propagation of radio        signals from global navigation satellite systems (GNSS) with its        electrically charged particles. This is a problem for the ever        higher precision required by these systems -- both in research        and for applications such as autonomous driving or precise orbit        determination of satellites.               Models of the ionosphere and its uneven, dynamic charge distribution        can help correct the signals for ionospheric delays, which are        one of the main error sources in GNSS applications. Researchers        have presented a new model of the ionosphere, developed on the        basis of neural networks and satellite measurement data from 19        years. In particular, it can reconstruct the topside ionosphere,        the upper, electron-rich part of the ionosphere much more        precisely than before. It is thus also an important basis for        progress in ionospheric research, with applications in studies on        the propagation of electromagnetic waves or for the analysis of        certain space weather events, for example.                      Facebook Twitter Pinterest LinkedIN Email              ==========================================================================       FULL STORY       ==========================================================================       The ionosphere -- the region of geospace spanning from 60 to 1000       kilometres above the Earth -- impairs the propagation of radio signals       from global navigation satellite systems (GNSS) with its electrically       charged particles.              This is a problem for the ever higher precision required by these systems       - - both in research and for applications such as autonomous driving or       precise orbit determination of satellites. Models of the ionosphere and       its uneven, dynamic charge distribution can help correct the signals       for ionospheric delays, which are one of the main error sources in       GNSS applications.              Researchers led by Artem Smirnov and Yuri Shprits of the GFZ German       Research Centre for Geosciences have presented a new model of the       ionosphere in the journal Nature Scientific Reports, developed on the       basis of neural networks and satellite measurement data from 19 years. In       particular, it can reconstruct the topside ionosphere, the upper,       electron-rich part of the ionosphere much more precisely than before. It       is thus also an important basis for progress in ionospheric research,       with applications in studies on the propagation of electromagnetic waves       or for the analysis of certain space weather events, for example.              Background: Importance and complexity of the ionosphere The Earth's       ionosphere is the region of the upper atmosphere that extends from       about 60 to 1000 kilometres in altitude. Here, charged particles such as       electrons and positive ions dominate, caused by the radiation activity of       the Sun -- hence the name. The ionosphere is important for many scientific       and industrial applications because the charged particles influence       the propagation of electromagnetic waves such as radio signals. The       so-called ionospheric propagation delay of radio signals is one of the       most important sources of interference for satellite navigation. This is       proportional to the electron density in the space traversed. Therefore,       a good knowledge of the electron density can help in correcting the       signals. In particular, the upper region of the ionosphere, above 600       kilometres, is of interest, since 80 per cent of the electrons are       gathered in this so-called topside ionosphere.              The problem is that the electron density varies greatly -- depending on       the longitude and latitude above the Earth, the time of day and year,       and solar activity. This makes it difficult to reconstruct and predict       them, the basis for correcting radio signals, for example.              Previous models There are various approaches to modelling electron density       in the ionosphere, among others, the International Reference Ionosphere       Model IRI, which has been recognised since 2014. It is an empirical       model that establishes a relationship between input and output variables       based on the statistical analysis of observations. However, it still has       weaknesses in the important area of the topside ionosphere because of       the limited coverage of previously collected observations in that region.              Recently, however, large amounts of data have become available for       this area.              Therefore, Machine learning (ML) approaches lend themselves to deriving       regularities from this, especially for complex non-linear relationships.              New approach using machine learning and neural networks A team from       the GFZ German Research Centre for Geosciences around Artem Smirnov,       PhD student and first author of the study, and Yuri Shprits, head of the       "Space Physics and Space Weather" section and Professor at University       Potsdam, took a new ML-based empirical approach. For this, they used       data from satellite missions from 19 years, in particular CHAMP, GRACE       and GRACE-FO, which were and are significantly co-operated by the GFZ,       and COSMIC. The satellites measured -- among other things -- the electron       density in different height ranges of the ionosphere and cover different       annual and local times as well as solar cycles.              With the help of Neural Networks, the researchers then developed a model       for the electron density of the topside ionosphere, which they call the       NET model.              They used the so-called MLP method (Multi-Layer Perceptrons), which       iteratively learns the network weights to reproduce the data distributions       with very high accuracy.              The researchers tested the model with independent measurements from       three other satellite missions.              Evaluation of the new model "Our model is in remarkable agreement with       the measurements: It can reconstruct the electron density very well in       all height ranges of the topside ionosphere, all around the Globe, at all       times of the year and day, and at different levels of solar activity,       and it significantly exceeds the International Reference Ionosphere       Model IRI in accuracy. Moreover, it covers space continuously," first       author Artem Smirnov sums up.              Yuri Shprits adds: "This study represents a paradigm shift in ionospheric       research because it shows that ionospheric densities can be reconstructed       with very high accuracy. The NET model reproduces the effects of       numerous physical processes that govern the dynamics of the topside       ionosphere and can have broad applications in ionospheric research."       Possible applications in ionosphere research The researchers see possible       applications, for instance, in wave propagation studies, for calibrating       new electron density data sets with often unknown baseline offsets,       for tomographic reconstructions in the form of a background model,       as well as to analyse specific space weather events and perform long-       term ionospheric reconstructions. Furthermore, the developed model can       be connected to plasmaspheric altitudes and thus can become a novel       topside option for the IRI.              The developed framework allows the seamless incorporation of new data       and new data sources. The retraining of the model can be done on a       standard PC and can be performed on a regular basis. Overall, the NET       model represents a significant improvement over traditional methods       and highlights the potential of neural network-based models to provide       a more accurate representation of the ionosphere for communication and       navigation systems that rely on GNSS.               * RELATED_TOPICS        o Earth_&_Climate        # Atmosphere # Weather # Geomagnetic_Storms #        Severe_Weather # Earth_Science # Climate #        Environmental_Issues # Geography        * RELATED_TERMS        o Ionosphere o Global_Positioning_System o Solar_cell o        Earth_science o Global_climate_model o Weather_forecasting o        Meteorology o Solar_power              ==========================================================================       Story Source: Materials provided by       GFZ_GeoForschungsZentrum_Potsdam,_Helmholtz_Centre. Note: Content may       be edited for style and length.                     ==========================================================================       Journal Reference:        1. Artem Smirnov, Yuri Shprits, Fabricio Prol, Hermann Lu"hr, Max        Berrendorf, Irina Zhelavskaya, Chao Xiong. A novel neural network        model of Earth's topside ionosphere. Scientific Reports, 2023; 13        (1) DOI: 10.1038/s41598-023-28034-z       ==========================================================================              Link to news story:       https://www.sciencedaily.com/releases/2023/04/230424103340.htm              --- up 1 year, 8 weeks, 10 hours, 50 minutes        * Origin: -=> Castle Rock BBS <=- Now Husky HPT Powered! (1:317/3)       SEEN-BY: 15/0 106/201 114/705 123/120 153/7715 218/700 226/30 227/114       SEEN-BY: 229/110 112 113 307 317 400 426 428 470 664 700 292/854 298/25       SEEN-BY: 305/3 317/3 320/219 396/45       PATH: 317/3 229/426           |
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