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Geomagnetic Measurements at the Pleshchenitsy Geophysical ObservatoryA significant long-term increase of some geomagnetic field components was revealed suggesting a
The Influence of Weak Geomagnetic Disturbances on the Rat Cardiovascular System under Natural and Shielded Geomagnetic Field Conditions of heart rate variability spectrum under natural and shielded geomagnetic field conditions. All tests were
Analysis of the magnetic storms and variations of the geomagnetic field components at the Pleshchenitsy ObservatoryAnalysis of the magnetic storms and variations of the geomagnetic field components
Evolution of the dipole geomagnetic field. Observations and models© 2016, Pleiades Publishing, Ltd.The works on paleomagnetic observations of the dipole geomagnetic
Analyzing the geomagnetic axial dipole field moment over the historical period from new archeointensity results at Bukhara (Uzbekistan, Central Asia) geomagnetic field models. These new data appear consistent with other Triaxe data previously obtained
Free core nutation: New large disturbance and connection evidence with geomagnetic jerks, which are also largely responsible for the geomagnetic field variations, particularly the geomagnetic
North-south asymmetry of geomagnetic and tropospheric events. There are the north-south asymmetry in the reaction of the geomagnetic field, of the geopotential and of the pressure
Free core nutation: New large disturbance and connection evidence with geomagnetic jerks, which are also largely responsible for the geomagnetic field variations, particularly the geomagnetic
Intermittence and peculiarities of a statistic characteristic of the geomagnetic field in geodynamo models of the geomagnetic field generated in the numerical geodynamo models has shown that the distribution of the spherical
Systematics of Early Cambrian Paleomagnetic Directions from the Northern and Eastern Regions of the Siberian Platform and the Problem of an Anomalous Geomagnetic Field in the Time Vicinity of the Proterozoic–Phanerozoic Boundary the predominant axial dipole component of the geomagnetic field, and necessitates the assumption
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