Variations in the Auroral Activity and Main Magnetic Field of the Earth over 300 years (1600–1909)

2018 ◽  
Vol 58 (6) ◽  
pp. 784-792 ◽  
Author(s):  
N. G. Ptitsyna ◽  
I. M. Demina ◽  
M. I. Tyasto
2020 ◽  
Author(s):  
Vincent Lesur ◽  
Aude Chambodut

<p>In magnetic observatories the Earth’s magnetic field is continuously recorded and the acquired data are calibrated so that the evolution of the field can be studied on time scales ranging from seconds to decades. The French network (the so called BCMT) includes 18 observatories around the world and the different types of data produced are freely accessible on several data centres. We will describe a typical infrastructure of a magnetic observatory, the measurement techniques, the instruments used, the general processing applied to obtain calibrated data and finally the environmental constraints that have to be respected in order to acquire suitable data. If magnetic observatories were originally set to monitor the slow variations of the Earth’s main magnetic field, they are more and more often used for space-weather monitoring and to study signal generated in the ionosphere and magnetosphere. This new range of applications implies an evolution of the network, of the acquisition and distribution techniques. The strategy we developed to respond to these new challenges will be also presented.</p>


2021 ◽  
Author(s):  
Agata Bury ◽  
Marek Lewandowski ◽  
Krzysztof Mizerski

AbstractIn this study, we investigated the geomagnetic ground observatory data from 1980 to 2011 collected from World Data Center from 134 stations. To analyze the data we have applied spherical harmonic decomposition to obtain components associated with the Earth’s main magnetic field and to calculate how the Earth’s dipole was varying in the aforementioned recent 31-year period. There is a visible ~ 2.3% decay of the dipole magnetic field of the Earth. We note that the present-day value of the magnetic dipole intensity is the lowest one in the history of modern civilization and that further drop of this value may pose a risk for different domains of our life.


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