The correct option is B Storage is proportional to outflow discharge
For the linear reservoir, storage varies linearly with the outflow discharge.
By Muskingum equation.
S=k[xIm+(1−x)Qm]
where, S= Storage of channel
I=Inflow rate
Q=Outflow rate
m=0.6(for artificial rectangular channel)
=1(for natural channel)
For natural channel,
S=k[xI+(1−x)Q]
where,
x=Weightage factor which ranges from 0 to 0.5.
For x=0,
S=f(Q)
Such a storage is known as linear storage or linear reservoir (or reservoir type storage) in which storage is only function of outflow discharge.
Note: Linear channel: The channels in which inflow hydrograph passes through a reach with only translation and no attenuation.