dc.creatorCordaro, E. G.
dc.creatorVenegas-Aravena, P.
dc.creatorLaroze, D.
dc.date.accessioned2019-10-11T17:29:59Z
dc.date.available2019-10-11T17:29:59Z
dc.date.created2019-10-11T17:29:59Z
dc.date.issued2019
dc.identifierAdvances in Space Research, Volumen 63, Issue 7, 2019, Pages 2290-2299
dc.identifier18791948
dc.identifier02731177
dc.identifier10.1016/j.asr.2018.12.019
dc.identifierhttps://repositorio.uchile.cl/handle/2250/171215
dc.description.abstract© 2018 COSPARWe report the existence of rapid variations in (effective) geomagnetic cutoff rigidity (Rc) between the equatorial and Antarctic zones adjacent to the Andes Mountains, revealed by the variation rate of geomagnetic cutoff rigidity (VRc) in the period 1975–2010. Our analysis is based on empirical records and theoretical models of the variations in cosmic rays and on the structure of geomagnetic fields. These have given us a different view of variations in Rc in time and space along the 70°W meridian, where secular variations in the geomagnetic field are strongly influenced by the proximity of the South Atlantic Magnetic Anomaly (SAMA), one of the most important characteristics of the terrestrial magnetic field that affects our planet, close from the equator to the 50°S parallel and from South America to South Africa. The VRc presents rapid changes in mid-latitudes where SAMA exerts its influence despite the existence of smooth changes in the geomagnetic field. This shows tha
dc.languageen
dc.publisherElsevier Ltd
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
dc.sourceAdvances in Space Research
dc.subjectAltiplano to Antarctica
dc.subjectGeomagnetic cutoff rigidity
dc.subjectGeomagnetic field
dc.subjectLatitudinal variation rate of geomagnetic cutoff rigidity
dc.subjectSouth Atlantic magnetic anomaly
dc.titleVariations of geomagnetic cutoff rigidity in the southern hemisphere close to 70°W (South-Atlantic Anomaly and Antarctic zones) in the period 1975–2010
dc.typeArtículo de revista


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