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dc.contributor.authorTsurutani, B.T.
dc.contributor.authorLakhina, G.S.
dc.date.accessioned2015-12-02T06:08:21Z
dc.date.accessioned2021-02-12T09:31:31Z-
dc.date.available2015-12-02T06:08:21Z
dc.date.available2021-02-12T09:31:31Z-
dc.date.issued2014
dc.identifier.citationGRL, v.41/2, p.287-292, 2014, doi: 10.1002/2013GL058825en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/728-
dc.description.abstractA “perfect” interplanetary coronal mass ejection could create a magnetic storm with intensity up to the saturation limit (Dst ~ −2500 nT), a value greater than the Carrington storm. Many of the other space weather effects will not be limited by saturation effects, however. The interplanetary shock would arrive at Earth within ~12 h with a magnetosonic Mach number ~45. The shock impingement onto the magnetosphere will create a sudden impulse of ~234 nT, the magnetic pulse duration in the magnetosphere will be ~22 s with a dB/dt of ~30 nT s−1, and the magnetospheric electric field associated with the dB/dt ~1.9 V m−1, creating a new relativistic electron radiation belt. The magnetopause location of 4 RE from the Earth's surface will allow expose of orbiting satellites to extreme levels of flare and ICME shock-accelerated particle radiation. The results of our calculations are compared with current observational records. Comments are made concerning further data analysis and numerical modeling needed for the field of space weather.en_US
dc.language.isoenen_US
dc.subjectCoronal mass ejectionen_US
dc.subjectMagnetosphereen_US
dc.subjectMagnetic stormen_US
dc.subjectInterplanetary coronal mass ejectionen_US
dc.subjectMagnetospheric electric fielden_US
dc.subjectICMEen_US
dc.titleAn extreme coronal mass ejection and consequences for the magnetosphere and Earthen_US
dc.typeArticleen_US
dc.identifier.accession091392
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