Long-period (30 days1 year) electromagnetic sounding and the electrical conductivity of the lower mantle beneath Europe |
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Authors: | Nils Olsen |
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Affiliation: | Danish Space Research Institute, Juliane Maries Vej 30, 2100 Copenhagen Ø, Denmark. E-mail: |
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Abstract: | The C -response connects the magnetic vertical component and the horizontal gradient of the horizontal components of electromagnetic variations and forms the basis for deriving the conductivitydepth profile of the Earth. Time-series of daily mean values at 42 observatories typically with 50 years of data are used to estimate C -responses for periods between 1 month and 1 yr. The Z : Y method is applied, which means that the vertical component is taken locally whereas the horizontal components are used globally by expansion in a series of spherical harmonics. In combination with results from previous analyses, the method yields consistent results for European observatories in the entire period range from a few hours to 1 yr, corresponding to penetration depths between 300 and 1800 km. 1-D conductivity models derived from these results show an increase in conductivity with depth z to about 2 S m-1 at z =800 km, and almost constant conductivity between z =800 and z =2000 km with values of 310 S m-1, in good agreement with laboratory measurements of mantle material. Below 2000 km the conductivity is poorly resolved. However, the best-fitting models indicate a further increase in conductivity to values between 50 and 150 S m-1. |
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Keywords: | electrical conductivity electromagnetic induction geomagnetic variations mantle |
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