Jamie Carter explains why Earth atmosphere delays true equal daylight

equinócio de primavera Foto: equinócio de primavera - Mike Pellinni/Shutterstock.com

The arrival of astronomical autumn across the Northern Hemisphere does not divide daytime and darkness into two identical portions of twelve hours each. Ground-level observers experience daylight that lingers for several minutes beyond the theoretical halfway mark on the exact date of the seasonal transition, delaying real mathematical parity until an event called the equilux. This observational divergence spans the celestial sphere and reshapes popular assumptions surrounding the scientific calendar.

Astronomers recorded the September equinox in 2026 on Tuesday, September 22 at 20:05 Eastern Daylight Time, corresponding to 00:05 Coordinated Universal Time on September 23. Science communicator Jamie Carter pointed out that this timing gap stems directly from the physical characteristics of Earth. Carter noted that “thanks in large part to Earth’s atmosphere, daylight will still outlast darkness for several minutes, with the true ‘equal night’ — known as the equilux — arriving a few days later”.

How planetary atmosphere and solar geometry prolong visible daylight

The divergence between geometric calculations and actual field observations originates from two core principles of optical physics and observational astronomy. The primary influence comes from atmospheric refraction caused by the gaseous envelope surrounding the globe, which refracts solar radiation much like an optical lens or glass prism. As sunlight travels through air layers that thin out toward space, the trajectory of the light curves toward the ground. This optical deflection lifts the apparent position of the sun by roughly 0.5 degrees near the horizon, allowing people on Earth to see the celestial body even when it sits geometrically beneath the line of sight.

Equinócio Primavera - Rui Elena/ shutterstock.com
Foto: Equinócio Primavera – Rui Elena/ shutterstock.com

British astronomer Stuart Clark, a contributor to The Guardian, detailed the visual mechanisms that alter official daily sunrise and sunset figures. Clark explained that “this happens because the Sun appears as a disc rather than a point of light, and the bending of its rays through our atmosphere means we can see it even when it is just below the horizon”. This bending of electromagnetic waves delivers surplus morning twilight and evening illumination across every terrestrial latitude.

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The second determining factor lies in the formal standards applied by international astronomical services to mark the start and end of each day. Dawn is not calculated when the geometric center of the sun crosses the horizon, but at the exact second the upper limb of the solar disk appears above the horizon line. Sunset concludes only when the topmost edge disappears completely beneath the horizon. Because the star must traverse its entire angular diameter before daytime officially ends, total visible daylight gains additional minutes compared to nighttime hours.

True twelve-hour balance arrives on the calendar through the equilux

Scientific terminology assigns the specific name equilux to the date that features twelve full hours of sunlight and twelve hours of darkness, combining the Latin words aequus, meaning equal, and lux, meaning light. The traditional word equinox derives instead from the union of aequus and nox, the Latin word for night. While historical etymology suggests a night of equal duration to the day, planetary optics consistently prevent that perfect symmetry during the orbital transition.

Achieving the equilux does not occur simultaneously across every continent, requiring location-specific calculations based on geographical latitude. Across temperate zones of the Northern Hemisphere, this absolute light balance typically takes place around four days after the date recorded on astronomical calendars. For observers located in major metropolitan areas such as Tokyo and Washington, astronomers calculated the autumn equilux of 2026 for Saturday, September 26, 2026.

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  • September 22, 2026: the Sun crosses the celestial equator heading south at 20:05 EDT.
  • September 23, 2026: official equinox occurs in Japan at 09:05 JST in tandem with the national Shūbun no Hi holiday.
  • September 26, 2026: equilux delivers twelve full hours of daytime illumination across Tokyo and Washington.
  • December 21, 2026: December solstice marks the longest night of the calendar year across the Northern Hemisphere.

Solar journey toward the south shortens daytime toward the December solstice

At the precise moment the equinox occurs in space, the Sun crosses the celestial equator on its apparent pathway toward southern celestial coordinates. During this orbital alignment, neither hemisphere leans toward the central star, keeping Earth axial tilt balanced relative to solar radiation. In Japan, the date of September 23 connects with the traditional holiday Shūbun no Hi, an annual public event focused on seasonal changes and honoring family ancestors.

Following the passage of the equilux in late September, the Northern Hemisphere registers nights that steadily exceed the daily duration of sunlight. This ongoing shortening of daylight continues without interruption through the autumn months until reaching the winter solstice on December 21, 2026. That astronomical milestone delivers the lowest levels of daily sunlight and the longest night of the entire annual cycle.

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