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dc.contributor.authorMaggiolo, R.
dc.contributor.authorMaes, L.
dc.contributor.authorCessateur, G.
dc.contributor.authorDarrouzet, F.
dc.contributor.authorDe Keyser, J.
dc.contributor.authorGunell, H.
dc.date2022
dc.date.accessioned2022-12-22T11:10:50Z
dc.date.available2022-12-22T11:10:50Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/10711
dc.descriptionThe presence of a large-scale planetary magnetic field is thought to be a protective factor for atmospheres, preventing them from being blown off by the solar wind. We focus on one key aspect of atmospheric escape: how does a planetary magnetic fields affect the energy transfer from the Sun to the atmosphere? We estimate the solar wind energy currently dissipated in the Earth's atmosphere using empirical formulas derived from observations. We show that it is significantly higher than the energy dissipated in the atmosphere of a hypothetical unmagnetized Earth. Consequently, we conclude that the Earth's magnetic field enhances the solar energy dissipation in the Earth's atmosphere and that, contrary to the old paradigm, an intrinsic magnetic field does not necessarily reduces atmospheric loss.
dc.languageeng
dc.titleThe Earth's Magnetic Field Enhances Solar Energy Deposition in the Upper Atmosphere
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.source.titleJournal of Geophysical Research: Space Physics
dc.source.volume127
dc.source.issue12
dc.source.pagee2022JA030899
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/2022JA030899
dc.identifier.scopus


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