- Hydromagnetic dynamos at the low Ekman and magnetic Prandtl numbers
Number of the records: 1  

Hydromagnetic dynamos at the low Ekman and magnetic Prandtl numbers

  1. 1.
    SYSNO ASEP0472505
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleHydromagnetic dynamos at the low Ekman and magnetic Prandtl numbers
    Author(s) Šimkanin, Ján (GFU-E) ORCID, RID
    Source TitleContributions to Geophysics & Geodesy - ISSN 1335-2806
    Roč. 46, č. 3 (2016), s. 221-244
    Number of pages24 s.
    Publication formOnline - E
    Languageeng - English
    CountrySK - Slovakia
    Keywordshydromagnetic dynamo ; magnetic Prandtl number ; inertial forces
    Subject RIVDE - Earth Magnetism, Geodesy, Geography
    OECD categoryPhysical geography
    R&D ProjectsLG13042 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Institutional supportGFU-E - RVO:67985530
    UT WOS000441852700004
    EID SCOPUS85011596002
    DOI https://doi.org/10.1515/congeo-2016-0014
    AnnotationHydromagnetic dynamos are numerically investigated at low Prandtl, Ekman and magnetic Prandtl numbers using the PARODY dynamo code. In all the investigated cases, the generated magnetic fields are dominantly-dipolar. Convection is small-scale and columnar, while the magnetic field maintains its large-scale structure. In this study the generated magnetic field never becomes weak in the polar regions, neither at large magnetic Prandtl numbers (when the magnetic diffusion is weak), nor at low magnetic Prandtl numbers (when the magnetic diffusion is strong), which is a completely different situation to that observed in previous studies. As magnetic fields never become weak in the polar regions, then the magnetic field is always regenerated in the tangent cylinder. At both values of the magnetic Prandtl number, strong polar magnetic upwellings and weaker equatorial upwellings are observed. An occurrence of polar magnetic upwellings is coupled with a regenaration of magnetic fields inside the tangent cylinder and then with a not weakened intensity of magnetic fields in the polar regions. These new results indicate that inertia and viscosity are probably negligible at low Ekman numbers.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2017
Number of the records: 1  

Metadata are licenced under CC0

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.