A long time ago, before scientists could measure the speed of light accurately, Ole Römer, a Danish astronomer, studied the eclipses of Jupiter's satellite Io. He was able to determine the speed of light from the observed periods of the satellite orbiting the planet Jupiter. Römer observed the time interval between two successive emergences of Io from behind the shadow of Jupiter.
Figure 1 shows the orbit of the Earth $E$ around the Sun $S$ and the orbit of Io (denoted by $M$) around the planet Jupiter. A long series of observations of the eclipses permitted an accurate evaluation of the orbital period $T_0=42~\text{h}~28~\text{min}~16~\text{s}$ of $M$.
The average distance of the Earth $E$ to the Sun is $R_E = 149.6 \cdot 10^6~\text{km}$. The period of revolution of the Earth is $T_E = 365~\text{days}$ and of Jupiter is $T_J = 11.86~\text{years}$. The distance of the satellite $M$ to the planet Jupiter is $R_M = 422 \cdot 10^3~\text{km}$.
Due to the finite speed of light, the period $T_\text{obs}$ between successive emergences observed from the Earth differs from $T_\text{real}$. An observer saw $M$ begin to emerge from the shadow at the moment $t$ when his position was at $\theta$ and the next emergence at the moment $t+T_\text{obs}$ when he was at $\theta+\Delta \theta$. Let us assume that $\theta=0$ for $t=0$.
Difference between maximal and minimal values of $T_\text{obs}$ is $\Delta T = 30~\text{s}$.