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Relation between the propagator matrix of geodesic deviation and the second-order derivatives of the characteristic function

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F13%3A10140175" target="_blank" >RIV/00216208:11320/13:10140175 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1080/09205071.2013.808595" target="_blank" >http://dx.doi.org/10.1080/09205071.2013.808595</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1080/09205071.2013.808595" target="_blank" >10.1080/09205071.2013.808595</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Relation between the propagator matrix of geodesic deviation and the second-order derivatives of the characteristic function

  • Original language description

    In the Finsler geometry, which is a generalization of the Riemann geometry, the metric tensor also depends on the direction of propagation. The basics of the Finsler geometry were formulated by William Rowan Hamilton in 1832. Hamilton's formulation is based on the first-order partial differential Hamilton-Jacobi equations for the characteristic function which represents the distance between two points. The characteristic function and geodesics together with the geodesic deviation in the Finsler space can be calculated efficiently by Hamilton's method. The Hamiltonian equations of geodesic deviation are considerably simpler than the Riemannian or Finslerian equations of geodesic deviation. The linear ordinary differential equations of geodesic deviationmay serve to calculate geodesic deviations, amplitudes of waves and the second-order spatial derivatives of the characteristic function or action. The propagator matrix of geodesic deviation contains all the linearly independent solution

  • Czech name

  • Czech description

Classification

  • Type

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

  • CEP classification

    DC - Seismology, volcanology and Earth structure

  • OECD FORD branch

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    Z - Vyzkumny zamer (s odkazem do CEZ)

Others

  • Publication year

    2013

  • 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 Electromagnetic Waves and Applications

  • ISSN

    0920-5071

  • e-ISSN

  • Volume of the periodical

    27

  • Issue of the periodical within the volume

    13

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    13

  • Pages from-to

    1589-1601

  • UT code for WoS article

    000322947700002

  • EID of the result in the Scopus database