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Kristian Snekvik

Researcher at University of Bergen

Publications -  48
Citations -  1135

Kristian Snekvik is an academic researcher from University of Bergen. The author has contributed to research in topics: Interplanetary magnetic field & Magnetosphere. The author has an hindex of 17, co-authored 48 publications receiving 921 citations. Previous affiliations of Kristian Snekvik include University of Helsinki & Finnish Meteorological Institute.

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Overview of Solar Wind–Magnetosphere–Ionosphere–Atmosphere Coupling and the Generation of Magnetospheric Currents

TL;DR: In this paper, the morphology and dynamics of the electrical current systems of the terrestrial magnetosphere and ionosphere were reviewed, and the conditions under which the currents are expected to be weak, and hence minimally contaminate measurements of the internally produced magnetic field of the Earth, were briefly outlined.
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How the IMF B-y induces a B-y component in the closed magnetosphere and how it leads to asymmetric currents and convection patterns in the two hemispheres

TL;DR: In this paper, the authors acknowledge the use of NASA/GSFC's Space Physics Data Data and the Facility for OMNI data, and provide results provided by the Community Coordinated Modeling Center at Goddard Space Flight Center through their public Run on Request (ROP) system (http://ccmc.gsfc.nasa.gov).
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How the IMF $\mathit{B}_{y}$ induces a $\mathit{B}_{y}$ component in the closed magnetosphere and how it leads to asymmetric currents and convection patterns in the two hemispheres

TL;DR: In this paper, the Lyon-Fedder-Mobarry global magnetohydrodynamics model was used to study the effects of the interplanetary magnetic field (IMF) IMF $\mathit{B}_{y}$ component on the coupling between the solar wind and magnetosphere-ionosphere system.
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Earthward plasma sheet flows during substorm phases

TL;DR: In this paper, the distribution of earthward plasma sheet flows during substorms was studied using 15 years of data obtained by Geotail, Cluster, and THEMIS, and the results indicated that any effect of the flows on substorm onset triggering would be caused by medium rather than very high speed flows.