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A revised corrected geomagnetic coordinate system for Epochs 1985 and 1990
Institution:1. Institute of Space Physics, Uppsala, S-75591, Sweden;2. World Data Center B2, Moscow, 117296, Russia;3. IZMIRAN, Troitsk, Moscow Region, 142092, Russia;1. Institute of Plant Nutrition and Natural Resources, Beijing Academy of Agriculture and Forestry Sciences, Beijing 100097, China;2. School of Electronic Information Engineering, Tianjin University, Tianjin 300072, China;3. School of Electronic Engineering, Tianjin University of Technology and Education, Tianjin 300222, China;1. Department of EEE, Hacettepe University, Beytepe, Ankara 06800, Turkey;2. IZMIRAN, Moscow, 142190 Troitsk, Russia;3. Department of EEE, Bilkent University, Bilkent, Ankara 06800, Turkey
Abstract:A new set of corrected geomagnetic coordinates (CGM) has been calculated from the magnetic field model DGRF for Epoch 1985 and the IGRF model for Epoch 1990. A new approach to determine the ‘dip’ magnetic equator has been developed, which is based on the vertical (along Re) projection on the Earth's surface of the B-minimum value point (apex) on each geomagnetic field line. A strip along the ‘dip’ magnetic equator line has been defined where the corrected geomagnetic coordinates could not be found by the definition of CGM. Linear interpolation between the locations of the two last definable CGM latitudes in both hemispheres has been used to calculate the CGM longitudes in the equatorial region. Interpolation between locations of the last definable CGM latitude and ‘dip’ equator in both hemispheres has been used to calculate the CGM latitudes in this region. The constant B-min geomagnetic coordinate system (CBM) is proposed and analysed to replace CGM in the equatorial region.
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