Angle of dip or inclination: Elements of Geomagnetism
An angle of Dip or inclination is the angle made with the horizontal by the Earth’s magnetic field lines. A wooden rod suspended by a torsion free thread from its center of gravity always remains horizontal (Figure). But a magnetic needle or a bar magnet similarly suspended will not come to rest in a horizontal position but will make some angle with the horizontal plane (Figure). This angle is called the angle of clip or inclination.
Definition: The angle between the direction of the earth’s magnetic field at a place and the horizontal direction measured in the plane of the magnetic meridian is called the angle of dip of the geomagnetism of that place. It is denoted by δ. The angle of dip is different at different places of the earth. If a suspended bar magnet is gradually taken towards the northern hemisphere, the north pole of the magnet will be found to dip more and more making gradual increase of angle with the horizontal downwards and in that case the angle of dip is written as δ°N or δ0 North or δ0 N. Again in the southern hemisphere the south pole of the magnet will dip downwards. In these positions, the angle of dip is written as δ°S or δ0 south or δ0 S. In the two poles dip is 90° and at the equator, it is 00.
Now the question arises why the magnetic axis of a freely suspended magnet does not remain horizontal other than at taw equation? We know, the earth is a huge magnet. So, there is a direction of the geomagnetic field intensity. It remains inclined with the horizontal other than that at the equator. Since freely suspended magnet aligns itself along the direction of the geomagnetic field intensity, hence the suspended magnet without remaining in the horizontal makes some angle with it.
Example: “Angle of dip of Dhaka is 31°N” means that if a bar magnet is suspended freely from its center of gravity, the north pole of the magnetic will remain hanging downward, and its magnetic axis will make an angle of 31° with the horizontal.