 Two-sided string data with zero slope

For the wave equation on a string, prescribing $y(0,t)=f(t)$ and $y_x(0,t)=0$ selects equal incoming and outgoing profiles. Write D'Alembert's formula as $P(t-x/c)+Q(t+x/c)$. The two traces imply $P+Q=f$ and $P^{\prime }=Q^{\prime }$, proving the displayed expression. These data do not generally describe a disturbance launched from an everywhere resting string. For nonsmooth $f$, derivatives and boundary traces need their piecewise classical or weak derivative interpretation; an endpoint cusp may prevent a classical derivative at an isolated time.