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Constraints on the lower mantle electrical conductivity from length-of-day changes

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F25%3A10510324" target="_blank" >RIV/00216208:11320/25:10510324 - isvavai.cz</a>

  • Result on the web

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=GMaMDsbv76" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=GMaMDsbv76</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.46298/jsedi.16005" target="_blank" >10.46298/jsedi.16005</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Constraints on the lower mantle electrical conductivity from length-of-day changes

  • Original language description

    We investigate how the radial profile 𝜎𝑚(𝑟 ) of the lower mantle electrical conductivity affectsthe downward continuation of the time-varying magnetic field to the core surface and the resulting invertedcore motions. We compare core flow predictions to the length-of-day (LOD) with geodetic records, in orderto assess how plausible the considered conductivity profiles are. The core flow inverse problem, mixing theinformation carried by single spherical harmonic magnetic coefficients, makes it non trivial to infer the delayexpected for LOD predictions. Our results indicate that the timescale characteristic of the mantle filter in thelow-frequency limit yields an integral measure of 𝜎𝑚(𝑟 ) allowing us to select admissible conductivity models.Models of 𝜎𝑚(𝑟 ) inferred from magnetospheric and tidal sources over the satellite era involve mantle filter lagsless than a couple of months and provide the best fit to LOD variations. Other conductivity profiles constructedbased on mineralogical properties and iron partitioning inferred for deep mantle rocks (i.e., 𝜎𝑚 increasing froma few S/m at 1200 km depth up to some tens of S/m TILDE OPERATOR+D91 300 km above the core surface, with a more conductingD&quot; layer) are acceptable. A highly conducting layer of thickness 𝑂(10 km) or thinner cannot be excluded.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>ost</sub> - Miscellaneous article in a specialist periodical

  • CEP classification

  • OECD FORD branch

    10500 - Earth and related environmental sciences

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Journal of studies of earth&apos;s deep interior

  • ISSN

  • e-ISSN

    3099-2877

  • Volume of the periodical

    1

  • Issue of the periodical within the volume

    paper 4

  • Country of publishing house

    FR - FRANCE

  • Number of pages

    17

  • Pages from-to

    1-17

  • UT code for WoS article

  • EID of the result in the Scopus database