mapbench

MapBench tool category

Sun & Moon Map Tools

Sunrise, sunset and day length. This hub groups 26 tools that answer related geographic questions while keeping the underlying method, data source and limitations visible.

Choose the tool that matches the question rather than the one with the most familiar name. Related tools can use different geographic models and legitimately return different answers.

View all 26 →

How to use this category well

Solar times use the NOAA algorithm with the 90.833° official zenith; lunar phase uses the synodic cycle. Timezone geometry comes from the open tz database resolved locally in your browser.

  • Convert solar times to local clock times deliberately: the sun keeps astronomical time, while governments keep political time, and the gap between them is large in many countries. State both when sharing results.
  • For photography, plan around sun altitude, not clock time: golden hour is an altitude band, so its clock time migrates with the seasons even at a fixed place — the calculator's windows handle that for you.
  • When comparing day length across a year, remember the curve is your latitude's signature: near-equatorial sites hover at twelve hours while high latitudes swing wildly. Choose expectations by latitude, not by calendar folklore.

Living by the sky: putting solar literacy to work

Solar literacy pays off in unglamorous, compounding ways: the photographer who plans by altitude windows instead of clock time stops losing light to season; the gardener who reads the daylight curve sets expectations by latitude, not by folklore; the distributed team that chooses its meeting slot from the overlap grid rotates pain instead of accumulating resentment; the traveller who checks polar behaviour avoids booking 'midnight sun' in a week the geometry never promised. None of this requires expertise — the arithmetic is exact and local — only the habit of carrying conventions along: which zenith, which clocks, which date. The sky keeps perfect books; the skill is quoting it with its units attached, and knowing the two doors (almanacs for science, terrain-aware tools for mountains) where everyday formulas hand over to specialists. There is also a quieter benefit to keeping this literacy in-house: because every computation runs locally, the tools become a classroom. Change a latitude and the daylight curve responds instantly; change a date and the golden-hour window migrates; add a second city and the overlap grid redraws. That immediacy turns parameters into intuitions in a way static tables never manage, which is why these pages invite play — drag the inputs, watch the geometry answer, and let the conventions (zenith, clocks, vintage) become habits rather than footnotes. A reader who has watched the polar circle snap day length to twenty-four hours understands something a definition alone cannot teach, and that understanding is the durable output of the whole exercise.

  • Add solar windows to trip notes as altitude ranges; convert to local time only at the end.
  • For teams, publish the overlap grid quarterly — DST changes move the rectangle more than anyone expects.
  • Garden planning: pair hardiness zone with the daylight curve; crops respond to both clocks.

Key terms

Declination

The sun's latitude-equivalent angle, ±23.44° across the year.

Equation of time

The sundial-vs-clock correction from orbit eccentricity and tilt.

Civil twilight

Sun between 0° and −6°: usable outdoor light without lamps.

Synodic month

The 29.53-day new-moon-to-new-moon cycle behind phases.

When to verify with an official source

MapBench is designed for analysis, learning and planning. If the result affects a legal boundary, surveying, emergency response, engineering, regulated eligibility, official statistics or a financial commitment, verify the underlying information with the responsible authority or qualified professional.