Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Tomáš ŠOLTIS"'
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 46, Iss 1, Pp 51-60 (2016)
The models of the distribution of the elements of the geomagnetic field must be updated regularly. For this purpose geomagnetic measurements have to be carried out repeatedly at geomagnetic observatories as well as at temporary observation points. In
Externí odkaz:
https://doaj.org/article/e4b75410f8354edab010d3ffc62e06c5
Autor:
Vladimír BEZÁK, Josef PEK, Dušan MAJCIN, Jana BUČOVÁ, Tomáš ŠOLTIS, Dušan BILČÍK, Radek KLANICA
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 45, Iss 1, Pp 1-11 (2015)
In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, for
Externí odkaz:
https://doaj.org/article/8d0738ec0e3947478e1df44d79777ec4
Autor:
Tomáš ŠOLTIS, Ján ŠIMKANIN
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 44, Iss 4, Pp 293-312 (2014)
We present an investigation of dynamo in a simultaneous dependence on the non-uniform stratification, electrical conductivity of the inner core and the Prandtl number. Computations are performed using the MAG dynamo code. In all the investigated case
Externí odkaz:
https://doaj.org/article/192db74284704073be81f12143c843da
Autor:
Tomáš ŠOLTIS, Jozef BRESTENSKÝ
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 43, Iss 4, Pp 271-303 (2013)
A linear stability analysis of convection arising in a horizontal plane layer rotating about the horizontal axis and permeated by a homogeneous horizontal magnetic field perpendicular to the rotation axis is performed. Resulting horizontal convective
Externí odkaz:
https://doaj.org/article/a82d856035fd4b8a80ba709f8f214449
Publikováno v:
Geophysical & Astrophysical Fluid Dynamics. 113:80-106
Turbulence in the Earth's outer core not only increases all diffusive coefficients, but it can lead to their anisotropic properties. Therefore, the model of rotating magnetoconvection in horizontal plane layer rotating about vertical axis and permeat
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 46, Iss 1, Pp 51-60 (2016)
The models of the distribution of the elements of the geomagnetic field must be updated regularly. For this purpose geomagnetic measurements have to be carried out repeatedly at geomagnetic observatories as well as at temporary observation points. In
Autor:
Tomáš Šoltis, Dušan Majcin, Jana Bučová, Dušan Bilčík, Josef Pek, Vladimír Bezák, Radek Klanica
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 45, Iss 1, Pp 1-11 (2015)
In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, for
Publikováno v:
Geophysical & Astrophysical Fluid Dynamics. 104:455-455