Seasons and sky
March Equinox
Direct answer
March Equinox: The March Equinox is the instant the Sun's apparent geocentric center crosses the celestial equator northward.
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At a glance
- Found in
- Seasons & Earth Almanac
- Related
- September Equinox, Astronomical Season, Equinox, Solstice
The March Equinox is the Sun's northward crossing of the celestial equator.
A Sun-Earth orientation for seasonal, atmospheric, tidal, and terrestrial terms.
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The story behind March Equinox
Equinox observations anchored calendars for millennia, while modern ephemerides calculate the crossing from precise solar coordinates.
Why March Equinox matters
March Equinox marks the astronomical start of Northern Hemisphere spring and Southern Hemisphere autumn while providing a precise global instant.
How to read March Equinox
March Equinox speaks to seasonal boundaries, equatorial solar geometry, and year-to-year almanac tables.
March Equinox in practice: an example
At the March Equinox the subsolar point crosses the equator from south to north.
Where readings of March Equinox go wrong
A common error is to expect exactly twelve hours of daylight everywhere; refraction, the solar disk, latitude, and terrain alter observed day length.
Sources and editorial method
Research references used for this entry include:
- NASA Science: Seeing Equinoxes and Solstices from Space - NASA explanation of axial tilt, the terminator, seasonal illumination, equinoxes, and solstices.
- U.S. Naval Observatory: Length of Day and Night at the Equinoxes - Official explanation of equinox geometry, refraction, and the difference between equinox and equilux.
- Source
- The Great Almanac Dictionary
- Category
- Seasons & Earth Almanac
- Last updated
- 2026-09-26
See the next northward crossing
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Common questions
What is the March Equinox?
The March Equinox is the instant the Sun's apparent geocentric center crosses the celestial equator northward.
What do people get wrong about the March Equinox?
A common error is to expect exactly twelve hours of daylight everywhere; refraction, the solar disk, latitude, and terrain alter observed day length.
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