The actual day of year and the latitude (0deg at the equator to 90deg at the North pole) both influence the length of the day.
The perceived way of the sun around the planet can be viewed at as the boundary circle of the planet's disc. However, this constellation (in which the sun apparently circles along the disc's boundary) applies only at equinoxes and only at the North pole. The further away one is from the North pole (towards the equator), the more the surrounding circle is tilted along the West-East axis, until it is completely upright (perpendicular to the planet's disc) at the equator.
Furthermore, there is also a shift of the circle away from the disc, along the obliquity of the ecliptic (connecting the centers of the two circles at an angle of 23.439deg). This shift can be "upwards" (max. distance at the summer solstice) or "downwards" (max. distance at the winter solstice) depending on the actual latitude.
The following image shows the tilted and shifted solar circle for the Winter Solstice at 45deg North. It is only the part b out of the whole circle in which the sun in visible: when continueing its path on the blue line it is night (but see the part titled#BTwilight below).
The sun does not appear or disappear just so, a shorter or longer twilight period beginsbefore the start of the day and endsafter the end of the day, i.e. the twilight affects the duration of the "dark" night, never the duration of the "bright" day.
For most purposes, it is sufficient to take into consideration theCivil Twilight plus theNautical Twilight, but not theAstronomical Twilight (which latter would be interpreted as fully dark anyway for casual observers).
Civil Twilight is defined as the sun being 6deg below the horizon, Nautical Twilight as 12deg. Therefore, the duration of the twilight depends on how long the sun needs to cross these 12deg, and this (mainly) depends from the angle the sun circle is tilted towards the planet's "disc". This angle is steep (orthogonal to the planet's disc) at the equator. The further away from the equator the observer is, the flatter the angle becomes, and there are Northern regions in which not the whole twilight cycle is completed. This is the case for all latitudes North of90deg-Axis-12deg=54.561deg.
To some extent the angle also depends from the day of year: It is at the equinoxes that the angle is steepest for any latitude, and on the Northern hemisphere the summer solstice is flattest (also the winter solstice is flatter than at the equinoxes, but not so flat as at the summer solstice). However, the differences along a year are short and extend over some minutes only.
Formulae
When the planet's so far flat disc is given some heighth, then twilight is defined as the parte of the solar arc.
This is the calculation of the twilight arc (comprising both twilight durationsand the daylength).
Then
completes the calculation.
Sample Values
Some individual twilight durationse (dusk or dawn) are given in the following tables. The tables' cells give the duration in hours.
Also note, that at and near the Pole there are phases with no twilight, because the sun is present all the day, or circles too far below the horizon. The values are given as 0, because half the difference between the daylength b and the arc comprising the day length and the 2 twilights((b+2e - b)/2)are presented. These values are identical at the pole (and near it), i.e. 0 around the winter solstice, and 1 around the summer solstice (0 and 24 hrs., resp.)
t=12deg
WS
Eq
SS
Eq
WS
Latitude/Day
0.00
45.66
91.31
136.97
182.63
228.28
273.94
319.59
365.25
90deg
0.000
0.000
12.000
0.000
0.000
0.000
12.000
0.000
0.000
80deg
0.000
4.158
6.000
0.000
0.000
0.000
6.000
4.158
0.000
70deg
3.685
2.903
2.562
2.343
0.000
2.343
2.562
2.903
3.685
60deg
1.977
1.723
1.677
2.608
2.755
2.608
1.677
1.723
1.977
50deg
1.359
1.293
1.287
1.499
1.788
1.499
1.287
1.293
1.359
45deg
1.204
1.166
1.166
1.295
1.436
1.295
1.166
1.166
1.204
40deg
1.092
1.070
1.074
1.157
1.237
1.157
1.074
1.070
1.092
30deg
0.948
0.941
0.947
0.985
1.015
0.985
0.947
0.941
0.948
20deg
0.867
0.866
0.872
0.888
0.900
0.888
0.872
0.866
0.867
10deg
0.826
0.827
0.831
0.837
0.841
0.837
0.831
0.827
0.826
0deg
0.818
0.818
0.818
0.818
0.818
0.818
0.818
0.818
0.818
The following table shows the twilight duration for the civil twilight (6deg rather than 12deg).