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Topography and geoid induced by a convecting mantle beneath an elastic lithosphere

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F12%3A10123815" target="_blank" >RIV/00216208:11320/12:10123815 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1111/j.1365-246X.2012.05364.x" target="_blank" >http://dx.doi.org/10.1111/j.1365-246X.2012.05364.x</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1111/j.1365-246X.2012.05364.x" target="_blank" >10.1111/j.1365-246X.2012.05364.x</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Topography and geoid induced by a convecting mantle beneath an elastic lithosphere

  • Original language description

    In the absence of seismological measurements, observations of the topography and gravity fields of solid planets are the primary constraints on their internal structure. To compute the synthetic geoid and topography induced by the dynamics of planetary interiors, we introduce a 3-D numerical tool describing mantle convection beneath an elastic lithosphere. Although the energy conservation is treated in the whole spherical domain, the deformation aspect is solved using a hybrid technique (finite volume method for the viscous flow, spectral method for elastic deformation). The mechanical coupling is achieved via the imposition of the traction at the surface of the viscous flow as a basal boundary condition for the elastic deformation. We present both response functions and full thermal convection cases computed with our new method for planetary bodies of varying dimensions: the filtering effect of the lithosphere on the dynamic topography and geoid is specific for each planetary body, ju

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DE - Earth magnetism, geodesy, geography

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

    Z - Vyzkumny zamer (s odkazem do CEZ)

Others

  • Publication year

    2012

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    GEOPHYSICAL JOURNAL INTERNATIONAL

  • ISSN

    0956-540X

  • e-ISSN

  • Volume of the periodical

    189

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    18

  • Pages from-to

    55-72

  • UT code for WoS article

    000301573800006

  • EID of the result in the Scopus database