Designed in Denmark by D. La Cour, over one hundred La Cour magnetographs were made by the Danish Meteorological Institute from 1926 onwards and were installed in French observatories in Terre Adélie and in Kerguelen in 1957 for International Geophysics Year. The La Cour variometers in Dumont d'Urville were in use until 1983.
The La Cour's magnetograph is an assemblage of fixed apparatus which detect and record variations in time of three different elements of the Earth magnetic field:
This set of fixed apparatus detects variations in time of three independent elements of the Earth magnetic field (H,D,Z or X,Y,Z). Each apparatus has a magnet with a flat mirror, and the mirror's rotations are proportional to the variations in the element considered. The indications given by these three apparatus can be recorded.
The variometers' sensitivity is determined using calibrating coils. Helmholtz coils are used, creating an easily calculable magnetic field during the passage of a continuous current of which the intensity is measured.
The H variometer, the Z variometer - also called the Godhavn balance - and the D variometer or "Copenhagen declinometer" were designed from 1926 onwards by D. La Cour. The Copenhagen declinometer is presented separately because it was never used in French observatories in austral and antartic regions.
Designed in Denmark by D. La Cour, over one hundred La Cour magnetographs were made by the Danish Meteorological Institute from 1926 onwards and were installed in French observatories in Terre Adélie and in Kerguelen in 1957 for International Geophysics Year. The La Cour variometers in Dumont d'Urville were in use until 1983.