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Question: To a man walking at the rate of 3 km/h, the rain appears to fall vertically. When he increases his s...

To a man walking at the rate of 3 km/h, the rain appears to fall vertically. When he increases his speed to 6 km/h, it appears to meet him at an angle of 45° with vertical. The speed of rain is

A

23\sqrt{3} km/h

B

6\sqrt{6} km/h

C

32\sqrt{2} km/h

D

43\sqrt{3} km/h

Answer

32\sqrt{2} km/h

Explanation

Solution

The problem involves relative motion, specifically the velocity of rain relative to a moving man. We can use vector addition/subtraction to solve this.

Let vR\vec{v}_R be the actual velocity of rain and vM\vec{v}_M be the velocity of the man. The velocity of rain relative to the man is given by vR/M=vRvM\vec{v}_{R/M} = \vec{v}_R - \vec{v}_M.

Let's assume the man walks along the positive x-axis and the rain has a horizontal component vxv_x and a vertical component vyv_y. So, vR=vxi^+vyj^\vec{v}_R = v_x \hat{i} + v_y \hat{j}. Since rain falls downwards, vyv_y will be negative.

Scenario 1:

The man walks at 3 km/h3 \text{ km/h}. So, vM=3i^\vec{v}_M = 3 \hat{i}.

The rain appears to fall vertically, which means its relative horizontal component is zero.

The relative velocity is vR/M=(vxi^+vyj^)3i^=(vx3)i^+vyj^\vec{v}_{R/M} = (v_x \hat{i} + v_y \hat{j}) - 3 \hat{i} = (v_x - 3) \hat{i} + v_y \hat{j}.

Since the rain appears to fall vertically, the horizontal component (vx3)(v_x - 3) must be zero.

vx3=0vx=3 km/hv_x - 3 = 0 \Rightarrow v_x = 3 \text{ km/h}.

So, the actual velocity of rain is vR=3i^+vyj^\vec{v}_R = 3 \hat{i} + v_y \hat{j}.

Scenario 2:

The man increases his speed to 6 km/h6 \text{ km/h}. So, vM=6i^\vec{v}_M' = 6 \hat{i}.

The rain appears to meet him at an angle of 4545^\circ with the vertical.

The new relative velocity is vR/M=vRvM=(3i^+vyj^)6i^=(36)i^+vyj^=3i^+vyj^\vec{v}_{R/M}' = \vec{v}_R - \vec{v}_M' = (3 \hat{i} + v_y \hat{j}) - 6 \hat{i} = (3 - 6) \hat{i} + v_y \hat{j} = -3 \hat{i} + v_y \hat{j}.

Let the horizontal component of vR/M\vec{v}_{R/M}' be vR/M,x=3 km/hv_{R/M,x}' = -3 \text{ km/h} and the vertical component be vR/M,y=vyv_{R/M,y}' = v_y.

The angle θ\theta with the vertical is given by tanθ=vR/M,xvR/M,y\tan \theta = \frac{|v_{R/M,x}'|}{|v_{R/M,y}'|}.

Given θ=45\theta = 45^\circ, we have tan45=3vy\tan 45^\circ = \frac{|-3|}{|v_y|}.

1=3vyvy=3 km/h1 = \frac{3}{|v_y|} \Rightarrow |v_y| = 3 \text{ km/h}.

Since rain falls downwards, vy=3 km/hv_y = -3 \text{ km/h}.

Now we have both components of the actual velocity of rain:

vR=3i^3j^\vec{v}_R = 3 \hat{i} - 3 \hat{j}.

The speed of rain is the magnitude of vR\vec{v}_R:

Speed of rain =vR=vx2+vy2=(3)2+(3)2= |\vec{v}_R| = \sqrt{v_x^2 + v_y^2} = \sqrt{(3)^2 + (-3)^2}

Speed of rain =9+9=18= \sqrt{9 + 9} = \sqrt{18}

Speed of rain =9×2=32 km/h= \sqrt{9 \times 2} = 3\sqrt{2} \text{ km/h}.