Sun Path Direction Table

58° to 120°where the sun rises at 40°N - a 62-degree swing across the year
Month (15th)Sunrise at 30°N40°N50°NSunset mirrors
January114°118°124°sunset same degrees south of west
February104°107°110°drifting back toward east
March92°93°93°equinox: due east, due west
April79°77°75°north of east begins
May68°65°60°northeast mornings
June62°58°52°solstice: widest north swing
July64°61°54°swing retreating
August73°71°67°still north of east
September86°85°84°second equinox: back to due east
October99°100°102°southeast mornings begin
November111°114°119°deep southeast
December117°120°127°solstice: widest south swing
Degrees run clockwise from true north - 90° is due east, 270° due west - and sunset mirrors sunrise about the north-south line, so the December sunrise at 120° southeast pairs a 240° southwest sunset. Computed from the same NOAA solar formulas as the daylight table, validated at the anchors: equinoxes land on due east at every latitude, and the solstice swing widens with latitude (52° at 50°N versus 62° at 30°N in June) because the sun's path tilts harder against a steeper horizon.
Who uses this: home buyers checking whether the winter sun clears the neighbor's roofline, gardeners placing beds before the shade map changes, photographers chasing the solstice alignments down city grids - Manhattanhenge is this table hitting a street grid. The single-date version lives at the sunrise sunset calculator, the duration column at the daylight by month table, and the panel-mounting consequences at the solar panel tilt table.

The sun rises due east exactly twice a year - and the rest of the time it drifts as much as sixty degrees north or south of that, depending on your latitude and the month. The table maps the full year of sunrise directions at three latitudes, with sunset mirroring the swing on the other side of the sky.

Bottom line: the swing widens with latitude. At 30°N the sun rises 62 degrees across the year; at 50°N it sweeps 75 - which is why northern summers feel endless in the evening (the sun sets far northwest) and northern winters feel dark by lunch (it rises far southeast and barely climbs). The equinoxes are the two honest reset points where every latitude agrees on due east.

The honest part: these are true-north degrees for a flat horizon, and the compass adds magnetic declination on top - a compass east is a few degrees off true east almost everywhere. Buildings and hills move the apparent sunrise along the horizon too, which is why the table describes the sun, not your street; the city-grid alignments like Manhattanhenge happen when this solar direction and the street layout briefly agree.

How to use

  1. Find your latitude's column and read the month: degrees run clockwise from true north (90 = east, 120 = southeast, 60 = northeast).
  2. Mirror the same degrees on the far side for sunset - a 120° sunrise travels with a 240° sunset the same day.
  3. For a real location, add your map's magnetic declination before pointing a compass, and let buildings argue with the horizon.
Good to know — Sunrise azimuth (clockwise from true north) swings 62 degrees across the year at 30°N, 75 at 50°N: due east (90°) only at the equinoxes, northeast minimum at the June solstice (52-62°), southeast maximum at the December solstice (117-127°). Sunset mirrors sunrise about north-south every day. Magnetic declination adds a compass correction on top; local horizons move the apparent event.
Quick reference — Use the table for the season, not the day: pick a window or a garden bed by where the low winter sun (December column) will actually shine, schedule the golden-hour shoot from the sunset mirror, and check the alignment dates off the solstices - the street-grid shows fall weeks away from them by design.

Frequently asked questions

What direction does the sunrise?

Due east - but only on the two equinoxes (late March and late September). Every other day the sunrise drifts: northeast from roughly April through August, southeast from roughly October through February, with the extremes at the solstices. At mid-latitudes the solstice sun rises about 30 degrees off east, which is a full third of the horizon's east half.

Why does the sunrise direction change through the year?

Earth's axis tips 23.4 degrees, so the sun's daily path slides north of the celestial equator in summer (rising north of east, arcing high, setting north of west) and south of it in winter (rising southeast, arcing low, setting southwest). The equinoxes are the two moments the path crosses the equator - the only days the sun rises due east everywhere on Earth, both hemispheres alike.

Does latitude change the sunrise direction?

Yes - higher latitudes see a wider swing. The June solstice sunrise runs 62° (northeast) at 30°N but 52° at 50°N, and the December one runs 117° to 127° southeast. The geometry: the axis tip tilts the sun's path harder against a steeper celestial horizon the further you stand from the tropics, which is the same leverage that makes northern summer days so long.

Where does the sun set in winter?

Southwest - the mirror of the southeast sunrise. At 40°N the December solstice sunset sits near 240° true (60 degrees south of west), which is why west-facing rooms lose their evening light in winter while south-facing ones keep theirs. The sunset swing equals the sunrise swing all year, reflected about the north-south line.

What is Manhattanhenge?

The twice-a-year evenings when the sunset's direction (near 250-260° in late May and mid-July at New York's latitude) aligns exactly with Manhattan's east-west street grid, lighting every cross street end to end. It is this table intersecting city planning: the grid was laid with a slight rotation off true east-west, so the alignment dates fall weeks off the solstice - and every grid city has its own version.

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