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Magnetic reconnection occurring between the interplanetary magnetic field and the dayside magnetopause causes a circulation of magnetic flux and plasma within the magnetosphere, known as the Dungey cycle. This circulation is transmitted to the ionosp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::abbdb6409d79bf1ecc717e87a58d93f9
https://doi.org/10.22541/essoar.168121412.21332677/v1
https://doi.org/10.22541/essoar.168121412.21332677/v1
Autor:
Stephen E. Milan, Jennifer Alyson Carter, Gemma E. Bower, Suzanne Mary Imber, Larry J. Paxton, Brian J. Anderson, Marc R. Hairston, Benoit Hubert
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c80a43e65ac9b36d0970874a77b28221
https://doi.org/10.1002/essoar.10503956.1
https://doi.org/10.1002/essoar.10503956.1