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dc.contributor.authorSolheim, Kristian Thinn
dc.contributor.authorJohnsen, Magnar Gullikstad
dc.date.accessioned2022-10-04T13:32:32Z
dc.date.available2022-10-04T13:32:32Z
dc.date.created2022-09-16T10:01:50Z
dc.date.issued2022
dc.identifier.isbn978-82-14-07588-5
dc.identifier.issn1504-9795
dc.identifier.urihttps://hdl.handle.net/11250/3023657
dc.description.abstractThis report focuses on geomagnetically induced currents (GIC) that can be induced in long subsea power cables. Literature indicates that the water depth itself, in which the cable will be laid, will not contribute to an attenuation of the geoelectric field for those water depths relevant for the Krafla power cable. However, the presence of a coast will introduce a strong enhancement. Even minor (<20 years) and moderate (~20-100 years) geomagnetic events can potentially cause considerable operational difficulty if sufficient mitigations are not in place. A close cooperation with Statnett (transmission system operator) is essential to limit any unintentional disconnection of the Krafla subsea cable.en_US
dc.description.abstractGeomagnetic induced currents in long subsea power cablesen_US
dc.language.isoengen_US
dc.publisherSINTEF Energi ASen_US
dc.relation.ispartofSINTEF Rapport
dc.relation.ispartofseriesSINTEF Rapport;
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titleGeomagnetic induced currents in long subsea power cablesen_US
dc.title.alternativeGeomagnetic induced currents in long subsea power cablesen_US
dc.typeResearch reporten_US
dc.description.versionpublishedVersionen_US
dc.rights.holderSINTEF Energi ASen_US
dc.source.pagenumber29en_US
dc.source.issue2022:00759en_US
dc.identifier.cristin2052338
cristin.ispublishedtrue
cristin.fulltextoriginal


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal