The mean angular radius of the Sun in radians is
$$ \frac{R_\odot}{\mathrm{au}}
= \frac{6.96 \times 10^5~\mathrm{km}}{1.496 \times 10^8~\mathrm{km}}
= 4.65 \times 10^{-3} $$
and its mean angular diameter is twice that, 0.00930 radian or 0.533°.
As the Earth's distance from the Sun annually varies by ±1.67%,
the Sun's angular diameter varies between 0.524° in July and 0.542° in January.
During a sunset, the Sun's altitude relative to the horizon decreases by that same angle.
If the observer is on the equator, the Sun goes straight down in just over 2 minutes as you would expect.
Otherwise the Sun descends at an oblique angle $q$, extending sunset by a factor of $1 / \sin q$.
For example, if $q$ is 30°, sunset takes twice as long as if $q$ were 90°.
If the observer's latitude is $\varphi$ and the Sun's declination is $\delta$, then
$$ q = \cos^{-1} \frac{\sin \varphi}{\cos \delta} $$
If $\delta \approx 0^\circ$, then $q \approx 90^\circ - \varphi$.
What changes at a nearly constant rate of 15°/hour is the Sun's hour angle relative to the meridian, measured around the celestial equator.
One degree of hour angle at declination $\delta$ spans only $\cos \delta$ degrees of sky, so the Sun appears to set about 8% slower in June and December than it does in March and September.