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dc.contributor.authorSolheim, Kristian Thinn
dc.contributor.authorJohnsen, Magnar Gullikstad
dc.date.accessioned2022-09-19T07:49:33Z
dc.date.available2022-09-19T07:49:33Z
dc.date.issued2022-09-16
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.descriptionSource at <a href=https://www.sintef.no/>https://www.sintef.no/</a>.en_US
dc.identifier.citationSolheim KT, Johnsen MG. Geomagnetic induced currents in long subsea power cables. SINTEF Energi AS; 2022. 29 p.. SINTEF Rapport(2022:00759)en_US
dc.identifier.cristinIDFRIDAID 2052338
dc.identifier.isbn978-82-14-07588-5
dc.identifier.urihttps://hdl.handle.net/10037/26852
dc.language.isoengen_US
dc.publisherSINTEF Energy Researchen_US
dc.relation.ispartofseriesSINTEF Rapport ; 2022:00759en_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2022 The Author(s)en_US
dc.titleGeomagnetic induced currents in long subsea power cablesen_US
dc.typeResearch reporten_US
dc.typeForskningsrapporten_US


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