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Интеллектуальная Система Тематического Исследования НАукометрических данных |
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The geotail inner edge position was estimated by THEMIS magnetic data with using A2000 and IGRF models and by projection the magnetic field line from the point of 30-80 keV protons izotropization boundary to the geotail during quiet and moderately disturbed geomagnetic conditions. It was found good correlation of these two methods.