Answer
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Hint:The dip angle, I, is the angle formed by the net field vector with respect to the flat plane, and it is positive for vectors below the plane. It's an exception to the standard polar angle of circular directions.
Complete answer:
The angle of dip, also known as the magnetic dip, is defined as the angle formed by the world's magnetic field lines intersecting the level. We also know that the angle of dip varies from highlight point to highlight point, providing information about the evolution of the world's magnetic field. When the magnetic field focuses downwards, the angle of dip should be positive. The angle of dip is expected to be negative as the magnetic field focuses upwards. We can deduce the following facts from the above definition:
While the dip needle rests evenly, the angle of dip is\[{0^0}\], and when the dip needle rests vertically, the angle of dip is\[{90^0}\]. The angle of dip is equal to \[{45^0}\] degrees when the flat and vertical segments of the world's magnetic field are identical. As a result, we can deduce that the angle of dip is the angle formed by the earth's magnetic field and the horizontal direction. The angle of dip is the angle formed by the complete intensity of the earth's magnetic field and a horizontal line in the magnetic meridian.
Note:The dip ranges from \[ - {90^0}\] (at the South Magnetic Pole) to \[ + {90^0}\] (at the North Magnetic Pole) (at the North Magnetic Pole). Isoclinic lines are shape lines along which the dip measured at the Earth's surface is equal.
Complete answer:
The angle of dip, also known as the magnetic dip, is defined as the angle formed by the world's magnetic field lines intersecting the level. We also know that the angle of dip varies from highlight point to highlight point, providing information about the evolution of the world's magnetic field. When the magnetic field focuses downwards, the angle of dip should be positive. The angle of dip is expected to be negative as the magnetic field focuses upwards. We can deduce the following facts from the above definition:
While the dip needle rests evenly, the angle of dip is\[{0^0}\], and when the dip needle rests vertically, the angle of dip is\[{90^0}\]. The angle of dip is equal to \[{45^0}\] degrees when the flat and vertical segments of the world's magnetic field are identical. As a result, we can deduce that the angle of dip is the angle formed by the earth's magnetic field and the horizontal direction. The angle of dip is the angle formed by the complete intensity of the earth's magnetic field and a horizontal line in the magnetic meridian.
Note:The dip ranges from \[ - {90^0}\] (at the South Magnetic Pole) to \[ + {90^0}\] (at the North Magnetic Pole) (at the North Magnetic Pole). Isoclinic lines are shape lines along which the dip measured at the Earth's surface is equal.
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