Approach using the log log diagnostic unit slope line:
A standard way pressure transient analysts recognize pure wellbore storage is by plotting $\log p_D$ against $\log t_D$ for early time drawdown data. During this period the data always falls on a straight line inclined at exactly 45 degrees, commonly called the unit slope line, because $p_D$ and $t_D$ are directly proportional to one another in this regime.
Writing the unit slope line algebraically:
A straight line of slope 1 on a log log plot means $\log p_D = \log t_D + \text{constant}$, which is the same as saying $p_D = (\text{constant}) \times t_D$. Physically, this constant of proportionality for the wellbore storage period is known from the material balance of the wellbore fluid to be $1/C_D$, so the unit slope line is described by $p_D = t_D / C_D$.
Checking the physical reasonableness:
This makes sense because a well with a very small storage coefficient $C_D$ (for example a well with a packer set near the perforations) will show a larger $p_D$ for a given $t_D$, since the wellbore has almost no capacity to buffer the pressure change, causing pressure to fall quickly. A well with a large $C_D$ (a long, fluid filled wellbore with no packer) buffers the pressure change more, so $p_D$ stays smaller for the same $t_D$. This inverse dependence of $p_D$ on $C_D$ at fixed $t_D$ is exactly what the relation $p_D = t_D/C_D$ predicts.
Solving for the required variable:
Cross multiplying the unit slope relation $p_D = t_D/C_D$ by $C_D$ on both sides isolates $t_D$ on one side, giving $t_D = p_D C_D$, which is the relation asked for in the question.
Final Answer:
\[ \boxed{t_D = p_D\,C_D} \]