When modeling the motion of point particles, you primarily used a Motion Graph to show, for example, the position of an object across many different instants in time. This sort of graph can still be used to show the motion of one position in a medium over time. This is known as a history graph.
When you have a history graph, a quantity of note is the period\(T\text{:}\) the time it takes to complete one full oscillation. As in simple harmonic motion, the period is related to the frequency by
\begin{equation*}
T = \frac{1}{f} = \frac{2\pi}{\omega}
\end{equation*}
Another quantity of note is the amplitude: the maximum displacement away from equilibrium of a particle in the medium.
Recall from simple harmonic motion the relationship between angular frequency, frequency, and period,
\begin{equation*}
\omega = 2 \pi f = \frac{2 \pi}{T}
\end{equation*}
Time is the physical quantity described by angular frequency, frequency, and period. There is an analogous spatial relationship between wavelength and a quantity called the wavenumber\(k\text{:}\)
\begin{equation*}
k = \frac{2 \pi}{\lambda}
\end{equation*}
The wavenumber represents the spatial frequency of a wave over a unit distance, and is measured in radians per meter.
A traveling wave propagates away from its source at a particular speed called the wave speed. Since both the period \(T\) and the wavelength \(\lambda\) correspond to a single cycle of a wave, they may be combined as follows:
\begin{equation*}
v = \mathrm{\frac{distance}{time}} = \frac{\lambda}{T} = \lambda f
\end{equation*}
However, it is worth noting that wave speed is not determined by the frequency of the wavelength. Instead, for mechanical waves, wave speed is a property of the medium’s elasticity! Combining this with knowledge of the frequency of the oscillating source allows you to determine the wavelength: