Golden Hour Calculator — Golden and Blue Hour Times for Any Location
The exact minutes the warm light starts and stops, for this morning and this evening, anywhere. Golden hour is defined here properly — the sun between the horizon and 6° above it — so you get the real duration for your latitude rather than a flat sixty minutes. The same page gives you blue hour, sunrise, sunset and solar noon, all three twilight tiers as dawn and dusk, day length and a year curve with the solstices and equinoxes marked.
Golden hour is almost never an hour
The name is a convention, not a measurement. Golden hour is the period when the sun sits between the horizon and about 6° above it, and how long that takes depends entirely on how steeply the sun climbs where you are standing.
| Place | Latitude | Evening golden hour, June | Evening golden hour, December |
|---|---|---|---|
| Singapore | 1° N | ~24 min | ~24 min |
| Cairo | 30° N | ~30 min | ~27 min |
| Brussels | 51° N | ~52 min | ~38 min |
| Reykjavík | 64° N | ~2 h+ | ~50 min |
Near the equator the sun drops almost vertically and the window is barely twenty-five minutes — if you are shooting in the tropics, arriving "about an hour before sunset" means arriving half an hour too early and then missing the end of it. In an Icelandic summer the sun skims along so shallowly that golden hour runs for hours and merges into the next one.
Morning golden hour is the one nobody uses
It is the same light, in reverse, and it has three advantages that get overlooked. The air is at its clearest before the day's haze and traffic build up. Locations are empty. And morning golden hour improves as it runs, so a late arrival still works, where in the evening every minute of hesitation costs you the best of it.
The catch is that you have to be in position before it starts, in the dark, which is why the blue hour time on this page matters as much as the golden hour one: it tells you when there will be enough light to find your footing.
Why the light goes warm at all
With the sun low, its light crosses far more atmosphere to reach you — at the horizon roughly forty times the path length it takes at noon. Air scatters short wavelengths much more strongly than long ones, so over that distance the blue is stripped out and what arrives is weighted towards red and orange. The colour temperature falls from about 5,500 K at midday to under 3,000 K.
The direction matters as much as the colour. Light arriving almost horizontally rakes across texture instead of flattening it, and the enormous scattering volume acts as a soft box, so shadows stay open. That combination — warm, directional, soft — is what no midday hour and no colour grade quite reproduces.