과제정보
This paper was modified and developed from a part of the Ph.D. thesis of the first author, which is submitted to and granted by the University of Alberta. This work was supported in part by a Canadian NSERC Discovery Grant to I.R.M. and partially by the Canadian Space Agency. CARISMA is operated by the University of Alberta, funded by the Canadian Space Agency (http://omniweb.gsfc.nasa.gov/). The authors thank I.R. Mann, D.K. Milling and the rest of the CARISMA team for data. CARISMA is operated by the University of Alberta, funded by the Canadian Space Agency. We thank the institutes who maintain the IMAGE Magnetometer Array: Tromso Geophysical Observatory of UiT the Arctic University of Norway (Norway), Finnish Meteorological Institute (Finland), Institute of Geophysics Polish Academy of Sciences (Poland), GFZ German Research Centre for Geosciences (Germany), Geological Survey of Sweden (Sweden), Swedish Institute of Space Physics (Sweden), Sodankyla Geophysical Observatory of the University of Oulu (Finland), Polar Geophysical Institute (Russia), and DTU Technical University of Denmark (Denmark). SAMNET is a UK PPARC National Facility operated by Lancaster University. The authors thank K. Shiokawa at Solar-Terrestrial Environment Laboratory, Nagoya University for the 210 MM chain magnetometer data. We thank the national institutes that support them and INTERMAGNET for promoting high standards of magnetic observatory practice (www.intermagnet.org). The GOES 8 magnetic field data are produced in real time by the NOAA Space Weather Prediction Center (SWPC) and are distributed by the NOAA National Geophysical Data Center (NGDC) (http://satdat.ngdc.noaa.gov/sem/goes/data/). We thank Geoff Reeves and the team at LANL for providing the SOPA data. This was supported by Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Education (NRF-2022R1A2C1092602).
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