Research related to international collaboration
FASSMER, Kathrin - KLONOWSKA, I. - WALCZAK, Katarzyna - ANDERSSON, B. - FROITZHEIM, Nikolaus - MAJKA, Jarosław - FONSECA, Raúl O. C. - MÜNKER, Carsten - JANÁK, Marian - WHITEHOUSE, Martin. Middle Ordovician subduction of continental crust in the Scandinavian Caledonides: an example from Tjeliken, Seve Nappe Complex, Sweden. In Contributions to Mineralogy and Petrology, 2017, vol. 172, no. 11-12, article Number 103. (2.913 - IF2016). (2017 - Current Contents). ISSN 0010-7999.
KLONOWSKA, I. - JANÁK, Marian - MAJKA, Jarosław - PETRÍK, Igor - FROITZHEIM, Nikolaus - GEE, David G. - SASINKOVÁ, Vlasta. Microdiamond on Åreskutan confirms regional UHP metamorphism in the Seve Nappe Complex of the Scandinavian Caledonides. In Journal of Metamorphic Geology, 2017, vol. 35, no. 5, p. 541-564. (3.594 - IF2016). (2017 - Current Contents). ISSN 0263-4929.
JORGENSEN, A. - HEILIG, Balázs - VELLANTE, Massimo - LICHTENBERGER, János - REDA, Jan - VALACH, Fridrich - MANDIC, Igor. Comparing the dynamic global core plasma model with ground-based plasma mass density observations. In Journal of Geophysical Research : Space Physics, 2017, vol. 122, no. 8, p. 7997-8013. (2.733 - IF2016). (2017 - Current Contents, WOS, SCOPUS). ISSN 2169-9380.
The DGCPM is a dynamical model of the flux-tube content in the plasmasphere which is widely used in space physics. The comparison of this model with the results of the observations of the plasma mass density made by means of the field-line resonance technique yielded relatively large disagreement. On the basis of data from the European quasi-meridional magnetometer array (EMMA), three of the parameters of the DGCPM were changed: characteristic time for depletion of the flux-tube, maximum flux from the ionosphere to the flux-tube, and saturation value of the plasma density. The functional form of the equations in the DGCPM as well as the other parameters of the model were preserved. For changing the parameters, only the data observed at the McIlwain L-value equal at 3.24 were used. Nonetheless, it turned out that the modified model well agrees also with the observations at other L-values.