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Illumination begins diminishing from western right limb
Epact (moon age on Jan 1): 12 days.
Historical North American Algonquin / Old Farmer folklore naming.
// 1. Julian Day (JD) at 2026-11-01 12:00 UTC
JD = 2461346.00 (Julian centuries T = 0.26834)
// 2. Synodic Lunar Age & Phase Angle
Delta Days from Epoch = (2461346.00 - 2460321.0) = 1025.00 d
Lunar Age = 20.96 days (of 29.53059d cycle)
Phase Angle φ = (20.96 / 29.53059) × 360° = 255.5°
Illumination k = [1 - cos(255.5°)] / 2 = 62.5% (Waning Gibbous)
// 3. Local Sidereal Time (LST) Alignment
LST = GMST (14:45:07) + (-74.01° / 15) = 09:49:06
Authoritative documentation conforming to the International Astronomical Union (IAU) 2000 Resolutions, NASA Eclipse Web Central, and the Astronomical Almanac.
The Moon does not orbit a static Earth. As the Moon travels around the Earth, the Earth simultaneously advances approximately $1^\circ$ per day along its heliocentric orbit around the Sun. This concurrent motion creates two distinct lunar orbital periods:
The illuminated fraction of the lunar disc k observable from Earth is calculated using the phase angle φ (the selenocentric angle between the Earth and the Sun):
Solar and lunar eclipses do not occur haphazardly; they follow a strict mathematical periodicity discovered by ancient Babylonian astronomers known as the Saros Cycle. An eclipse can only occur when the Moon is simultaneously at syzygy (New or Full) and crossing the plane of the ecliptic at one of its orbital nodes (ascending or descending node).
The Saros cycle represents the harmonic resonance among three distinct lunar orbital frequencies:
Because these three periods coincide within fractions of a day after 6,585.32 days (18 years, 11 days, 8 hours), an eclipse with nearly identical geometry, magnitude, and totality duration recurs in the same Saros family. The remaining 8 hours (0.321 days) causes the Earth to rotate 120° west, shifting the eclipse path one-third of the globe westward on every successive cycle. After three Saros cycles (54 years and 34 days, known as an Exeligmos), the eclipse returns to approximately the same geographic longitude.
A pure solar year (tropical year) contains 365.2422 days, while a pure lunar year of 12 synodic months contains only 12 × 29.53059 = 354.3671 days. This fundamental discrepancy of 10.875 days per year (known as the annual epact) causes lunar calendars (such as the Islamic Hijri calendar) to drift backward through the solar seasons by roughly 11 days each year.
Lunisolar calendars (such as the Hebrew, traditional Chinese, and Hindu calendars) reconcile this drift using the Metonic Cycle, documented by Meton of Athens in 432 BCE:
The two cycles align with an astonishing precision of just 2 hours over 19 years! To maintain synchronization, lunisolar calendars insert seven intercalary leap months (embolisms) across each 19-year cycle (specifically in years 3, 6, 8, 11, 14, 17, and 19).
While civil clocks follow the Sun, observational astronomers and telescope mounts operate on Sidereal Time. A sidereal day is the time required for Earth to rotate 360° on its axis relative to the vernal equinox (23h 56m 4.091s of mean solar time).
Local Sidereal Time (LST) is fundamentally equal to the Right Ascension (RA) of any celestial object currently crossing the observer's local meridian. By setting a telescope's equatorial setting circles or computerized GoTo drive to the current LST, objects at transit can be targeted with zero hour angle (HA = LST - RA = 0).
Because the Moon's orbit is elliptical (e = 0.0549), its distance from Earth ranges from perigee (363,300 km) to apogee (405,500 km). A Full Moon occurring within 90% of closest perigee is colloquially known as a Supermoon; it appears approximately 14% larger in apparent diameter and 30% brighter in luminous flux than an apogee Micromoon.
The Moon's orbital plane is inclined by 5.14° relative to the plane of the Earth's orbit around the Sun (the ecliptic). At most New and Full Moons, the Moon passes safely above or below the Sun, casting its shadow harmlessly into empty space. Eclipses can only transpire during eclipse seasons, when the Sun is near one of the Moon's orbital nodes.
The Moon is in 1:1 spin-orbit tidal resonance (tidal locking) with Earth. Over billions of years, Earth's gravitational tidal torque slowed the Moon's rotational period until it matched its orbital period (27.32 days). Observers see slight edge wobbles (up to 59% of the total lunar surface over time) due to lunar optical librations.
Calculate next solar eclipse dates. Designed for fast, accurate calculation with clear outputs, explanation, and device-friendly usability.
Illumination begins diminishing from western right limb
Epact (moon age on Jan 1): 12 days.
Historical North American Algonquin / Old Farmer folklore naming.
// 1. Julian Day (JD) at 2026-11-01 12:00 UTC
JD = 2461346.00 (Julian centuries T = 0.26834)
// 2. Synodic Lunar Age & Phase Angle
Delta Days from Epoch = (2461346.00 - 2460321.0) = 1025.00 d
Lunar Age = 20.96 days (of 29.53059d cycle)
Phase Angle φ = (20.96 / 29.53059) × 360° = 255.5°
Illumination k = [1 - cos(255.5°)] / 2 = 62.5% (Waning Gibbous)
// 3. Local Sidereal Time (LST) Alignment
LST = GMST (14:45:07) + (-74.01° / 15) = 09:49:06
Authoritative documentation conforming to the International Astronomical Union (IAU) 2000 Resolutions, NASA Eclipse Web Central, and the Astronomical Almanac.
The Moon does not orbit a static Earth. As the Moon travels around the Earth, the Earth simultaneously advances approximately $1^\circ$ per day along its heliocentric orbit around the Sun. This concurrent motion creates two distinct lunar orbital periods:
The illuminated fraction of the lunar disc k observable from Earth is calculated using the phase angle φ (the selenocentric angle between the Earth and the Sun):
Solar and lunar eclipses do not occur haphazardly; they follow a strict mathematical periodicity discovered by ancient Babylonian astronomers known as the Saros Cycle. An eclipse can only occur when the Moon is simultaneously at syzygy (New or Full) and crossing the plane of the ecliptic at one of its orbital nodes (ascending or descending node).
The Saros cycle represents the harmonic resonance among three distinct lunar orbital frequencies:
Because these three periods coincide within fractions of a day after 6,585.32 days (18 years, 11 days, 8 hours), an eclipse with nearly identical geometry, magnitude, and totality duration recurs in the same Saros family. The remaining 8 hours (0.321 days) causes the Earth to rotate 120° west, shifting the eclipse path one-third of the globe westward on every successive cycle. After three Saros cycles (54 years and 34 days, known as an Exeligmos), the eclipse returns to approximately the same geographic longitude.
A pure solar year (tropical year) contains 365.2422 days, while a pure lunar year of 12 synodic months contains only 12 × 29.53059 = 354.3671 days. This fundamental discrepancy of 10.875 days per year (known as the annual epact) causes lunar calendars (such as the Islamic Hijri calendar) to drift backward through the solar seasons by roughly 11 days each year.
Lunisolar calendars (such as the Hebrew, traditional Chinese, and Hindu calendars) reconcile this drift using the Metonic Cycle, documented by Meton of Athens in 432 BCE:
The two cycles align with an astonishing precision of just 2 hours over 19 years! To maintain synchronization, lunisolar calendars insert seven intercalary leap months (embolisms) across each 19-year cycle (specifically in years 3, 6, 8, 11, 14, 17, and 19).
While civil clocks follow the Sun, observational astronomers and telescope mounts operate on Sidereal Time. A sidereal day is the time required for Earth to rotate 360° on its axis relative to the vernal equinox (23h 56m 4.091s of mean solar time).
Local Sidereal Time (LST) is fundamentally equal to the Right Ascension (RA) of any celestial object currently crossing the observer's local meridian. By setting a telescope's equatorial setting circles or computerized GoTo drive to the current LST, objects at transit can be targeted with zero hour angle (HA = LST - RA = 0).
Because the Moon's orbit is elliptical (e = 0.0549), its distance from Earth ranges from perigee (363,300 km) to apogee (405,500 km). A Full Moon occurring within 90% of closest perigee is colloquially known as a Supermoon; it appears approximately 14% larger in apparent diameter and 30% brighter in luminous flux than an apogee Micromoon.
The Moon's orbital plane is inclined by 5.14° relative to the plane of the Earth's orbit around the Sun (the ecliptic). At most New and Full Moons, the Moon passes safely above or below the Sun, casting its shadow harmlessly into empty space. Eclipses can only transpire during eclipse seasons, when the Sun is near one of the Moon's orbital nodes.
The Moon is in 1:1 spin-orbit tidal resonance (tidal locking) with Earth. Over billions of years, Earth's gravitational tidal torque slowed the Moon's rotational period until it matched its orbital period (27.32 days). Observers see slight edge wobbles (up to 59% of the total lunar surface over time) due to lunar optical librations.
Calculate next solar eclipse dates. Designed for fast, accurate calculation with clear outputs, explanation, and device-friendly usability.