The angle of elevation of a cloud from a point h metre above a lake is θ. The angle of depression of its reflection in the lake is 45∘. The height of the cloud is :
h(1+tan θ1−tan θ)
Let H metre be the height of the could above water level. The distance of the reflection is same as that of the cloud from the lake surface.
Here, AB = h, AC = BQ = x
In ΔACP, tan θ=PCAC=H−hx
⇒x=H−htan θ ... (1)
In ΔACR, tan 45∘=RCAC=H+hx
⇒x=H+htan 45∘
⇒x=H+h ... (2)
From (1) and (2), we have
(H+h)(tan θ)=(H−h)⇒H(1−tan θ)=h(1+tan θ)
⇒H=h(1+tan θ1−tan θ)