The ascent of the summer lines of temperature to the west is explained by the diminution of magnetic intensity.
Some observations for the magnetic intensity were obtained at this station.
This is most obvious, if not most influential, where the magnetic intensity is greatest.
The movement of the area of magnetic intensity, and the magnetic pole, to the west.
The effect of this difference of magnetic intensity upon the climate of Europe is marked.
|magnetic intensity |
See magnetic field strength.