Question
Question: The horizontal component of the earth’s magnetic field at a place is B and the angle of dip is \({60...
The horizontal component of the earth’s magnetic field at a place is B and the angle of dip is 60∘. What is the value of the vertical component of the earth’s magnetic field at the equator?
Solution
Hint: In this question, we start with the horizontal and vertical components of the earth’s magnetic field that is MH=Mcos(δ) and MV=Msin(δ) respectively. Then we equate the horizontal component of the earth’s magnetic field to B and substitute δ=60∘ in MH=Mcos(δ) and we get M=2B. Now to find the vertical component of the magnetic field at the equator we substitute M=2B and δ=60∘ in MV=Msin(δ) and get MV=0 at the equator.
Complete step-by-step answer:
In this question, it is given that the horizontal component of the earth’s magnetic field at a location is B. Also, the dip at the same location is δ=60∘
So we first draw the figure shown below to have a better understanding
Now let us assume that the earth’s magnetic field M, so
The horizontal component will be MH=Mcos(δ)------ (1)
The vertical component will be MV=Msin(δ) -------- (2)
But it is given that horizontal component is B, so using equation (1) we get
MH=Mcos(δ)=B------------------------------- (3)
Substituting δ=60∘ in equation (3), we will get
B=Mcos(60∘)
⇒B=M×21
⇒M=2B ------------------------------------- (4)
Now we know that at the equator the dip becomes zero, that is δe=0∘. So substituting δe=0∘ and M=2B in equation (2), we will get the vertical component of the magnetic field at the equator that is
MV=Msin(δe)
⇒MV=2Bsin(0∘)
⇒MV=2B×0
⇒MV=0
Hence the vertical component of the magnetic field at the equator of the earth is 0.
Note: For these types of questions we need to know what is Geographical meridian and magnetic meridian. We also need to know how to calculate the horizontal component and vertical component of the earth’s magnetic field. We should also know what is the angle of declination and angle of dip and how they vary at a different position on Earth’s surface.