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Moon Illumination Fraction

This tells you what fraction of the Moon's visible disk is lit by the Sun at any moment. It is calculated from the phase angle, the Sun-Moon-Earth angle: k = (1 + cos θ) / 2. When θ = 0° (full moon), k = 1, meaning 100% illuminated. When θ = 180° (new moon), k = 0. The fraction changes smoothly through the month. It is used by astronomers planning observations and by anyone wanting to know how bright the Moon will be tonight.

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VORZEP · LUNAR & CELESTIAL MECHANICS TOOLS

Moon Illumination Fraction Calculator

Solve the classic lunar-phase relation k = (1 + cos θ) / 2 for either of its two unknowns — the illuminated fraction or the phase angle — with step-by-step math, a live Sun–Earth–Moon geometry diagram, the Moon as it appears from Earth, and companion metrics including phase name, lunar age and elongation.

k = (1 + cos θ) / 2 · θ = phase angle (Sun–Moon–Earth)
Solve for
Waxing or waning?
Illuminated Fraction (k) The fraction of the Moon's disc that appears illuminated as seen from Earth, ranging from 0 at New Moon to 1 at Full Moon. Sometimes reported as a percentage (0 – 100%). It is not the same as the illuminated hemisphere — the Sun always lights half the Moon, but we see varying amounts of that lit half. Values: 0 = New, 0.25 = Crescent, 0.5 = Quarter, 0.75 = Gibbous, 1 = Full.
0 – 1
Illuminated fraction must be between 0 and 1.
= 75.00% illuminated · Gibbous · θ = 60.00°
Phase Angle (θ) The Sun–Moon–Earth angle at the Moon's centre. θ = 0° corresponds to Full Moon (Sun and Earth in the same direction from the Moon, so the fully lit hemisphere faces Earth). θ = 180° corresponds to New Moon (Sun and Earth in opposite directions from the Moon). θ = 90° is a Quarter Moon. Range: 0° – 180°.
°
Phase angle must be between 0° and 180°.
= 60.00° · 1.0472 rad · k = 0.7500
ILLUMINATED FRACTION (k)
0.7500
75.00% illuminated · θ = 60.00° · Waxing Gibbous
WAXING GIBBOUS
k = (1 + cos θ) / 2
Step-by-step solution
Illuminated fraction k vs. phase angle θ
k = (1 + cos θ) / 2 Current phase angle θ
Lunar phase gallery across θ = 0° → 180°
Appearance at each phase angle, with illuminated fraction shown
Lunar age through the synodic month
Lunar age in days (from New Moon) Current age
Sensitivity
Companion lunar metrics
Elongation, age & timing
Sun–Earth–Moon geometry & the Moon as seen from Earth
SUN–EARTH–MOON GEOMETRY · k = (1 + cos θ) / 2 · θ = Sun–Moon–Earth angle SUN (direction of light →) EARTH sunlight → MOON ψ θ θ = 60.00° · ψ = 120.00° AS SEEN FROM EARTH Waxing Gibbous k = 0.7500 (75.00%) θ = 60.00° · age ≈ 11.1 d lit side orientation shown for Northern Hemisphere (mirror left–right for Southern Hemisphere) k = (1 + cos 60.00°) / 2 = (1 + 0.5000) / 2 = 0.7500
Sunlight direction — always lights exactly half the Moon's surface Earth — location of the observer Moon's illuminated fraction k as seen from Earth Elongation ψ (Sun–Earth–Moon) distinguishes waxing from waning
What the illuminated fraction really measures
killuminated fraction
=
(1 + cos θ)half of the sum
/
2normalisation

The Sun always lights half the Moon

The single most important thing to understand about lunar phases is that the Sun always illuminates exactly one hemisphere of the Moon — the hemisphere facing the Sun. What changes through the month is the angle from which we see that lit hemisphere. When Earth is between the Sun and the Moon (Full Moon), we see the entire lit hemisphere, so k = 1. When the Moon is between Earth and the Sun (New Moon), we see only the dark side, so k = 0. The illuminated fraction k is a purely geometric consequence of the phase angle θ.

Quarter Moon is exactly half lit

At First or Last Quarter, θ = 90°, so cos θ = 0, so k = 0.5 — exactly half the visible disc is lit. This is why "quarter" Moon is a slightly confusing name: only half of the visible face is illuminated, even though the Moon has completed one quarter of its synodic cycle since New Moon. The term "quarter" refers to the phase (one quarter of the cycle), not to the illuminated fraction. A half-lit Moon is a quarter-phase Moon, not a "half moon".

k changes fastest near the quarters

The derivative dk/dθ = −sin θ / 2 is zero at Full and New Moon (θ = 0° or 180°), where the illumination changes most slowly, and reaches its maximum magnitude at the quarters (θ = 90°). This is why the Moon near First Quarter appears to change shape noticeably from one night to the next, while near Full Moon it stays visually "full" for several nights in a row. The same slow variation near Full explains why the two or three brightest nights of the month look almost identical.

Waxing and waning are mirror images

For every value of k between 0 and 1, there are two distinct phases: one waxing (growing) and one waning (shrinking), separated by roughly half a synodic month. The formula k = (1 + cos θ) / 2 cannot distinguish between them — it depends only on the magnitude of the phase angle, not on which side of the cycle the Moon is on. This is why the calculator has a waxing/waning toggle: it does not change k or θ, but it determines which side of the Moon appears lit as seen from Earth, and therefore the phase name and the lunar age.

How to Use This Calculator

The illuminated-fraction relation links two quantities: k and θ. Pick which one you want the tool to solve, choose waxing or waning, then fill in the value.

1. Choose what to solve for

Pick k or θ from the toggle. The calculator rearranges k = (1 + cos θ)/2 — solving θ = arccos(2k − 1) when you know the illuminated fraction.

2. Select waxing or waning

k alone does not determine which side of the Moon is lit — you need to tell the calculator whether the Moon is growing toward Full (waxing) or shrinking toward New (waning). This affects the phase name, the lunar age, and the orientation of the rendered Moon.

3. Use realistic presets

Presets jump straight to the standard phases: New, Crescent, Quarter, Gibbous, and Full Moon, plus the corresponding phase angles of 0°, 45°, 60°, 90°, 135° and 180°. The default is a Waxing Gibbous at k = 0.75.

4. Read the result and verdict

The result card shows k as a decimal and a percentage, the phase angle θ in degrees, and the lunar phase name. A colour-coded badge classifies the phase from New through the crescent/quarter/gibbous stages up to Full.

5. Check the geometry and appearance panels

The diagram shows the Sun–Earth–Moon configuration from above with the phase angle θ and elongation ψ drawn explicitly, and a live rendering of the Moon as it appears from Earth, oriented for the Northern Hemisphere. The illuminated region updates continuously as you drag the slider.

6. Switch to Advanced for depth

Advanced mode adds a phase gallery across θ = 0° to 180°, a lunar-age curve, a sensitivity analysis, and companion metrics including elongation, illuminated fraction, lunar age in days, and percentage of the synodic cycle completed.

What This Tool Offers

Built around the classic lunar-phase relation k = (1 + cos θ) / 2, the geometric core of the Moon's monthly cycle.

Two-way solving

Solve for the illuminated fraction k or the phase angle θ. The calculator rearranges k = (1 + cos θ)/2 in both directions, using arccos to recover θ from k.

Live Sun–Earth–Moon geometry

A top-down view of the Sun, Earth and Moon with the orbit, sunlight direction, elongation arc ψ and phase angle arc θ drawn explicitly at every update.

Real-time Moon rendering

The Moon as it appears from Earth, with the correct illuminated fraction, lit-side orientation for waxing or waning, subtle crater hints, and a live phase-name caption.

Derived hints everywhere

Each field shows the value converted to related units — k as a percentage, θ in degrees and radians, the implied phase name, and the current lunar age in days.

Three linked charts

k vs θ across the full phase range, a phase gallery rendering the Moon at nine different θ values, and a lunar-age curve showing the progression from New to Full and back.

Reference tables

A phase reference table mapping k, θ, elongation, age and appearance; a synodic-month timeline; and a variable reference with formula notes.

Reference Tables & Conversions

A phase lookup table, the synodic month timeline, and a variable reference.

Phase lookup table

Phaseθ (°)k% litElongation ψAge (days)
New Moon1800.0000%0°0.00
Waxing Crescent (early)157.50.0383.8%22.5°1.85
Waxing Crescent (mid)1350.14614.6%45°3.69
Waxing Crescent (late)112.50.30930.9%67.5°5.54
First Quarter900.50050.0%90°7.38
Waxing Gibbous67.50.69169.1%112.5°9.23
Waxing Gibbous (late)450.85485.4%135°11.07
Waxing Gibbous (nearly Full)22.50.96296.2%157.5°12.92
Full Moon01.000100%180°14.77
Waning Gibbous22.50.96296.2%202.5°16.61
Waning Gibbous (mid)67.50.69169.1%247.5°20.30
Last Quarter900.50050.0%270°22.15
Waning Crescent1350.14614.6%315°25.84
Waning Crescent (late)157.50.0383.8%337.5°27.68

The Synodic Month

The Moon completes one full cycle of phases in 29.53059 days — the synodic month. Because the Earth is also orbiting the Sun during this time, the synodic month is about 2.2 days longer than the Moon's true orbital period (the sidereal month of 27.32166 days). The difference is the time it takes the Moon to "catch up" with the Sun's apparent motion across the sky.

QuantityValueNotes
Synodic month29.53059 daysMean time from New Moon to New Moon
Sidereal month27.32166 daysTrue orbital period relative to the stars
Anomalistic month27.55455 daysPerigee to perigee (elliptical orbit)
Draconic month27.21222 daysNode to node (eclipse cycle)
Mean daily elongation12.19° / day360° / 29.53059
Mean k change per day~0.10Fastest near the quarters, slowest near Full/New

Variable Reference

SymbolMeaningTypical rangeUnits
kIlluminated fraction of the Moon's visible disc0 – 1dimensionless
θPhase angle (Sun–Moon–Earth)0 – 180degrees
ψElongation (Sun–Earth–Moon)0 – 360degrees
ageDays since New Moon0 – 29.53days
TSynodic month29.53059days
DMoonAngular diameter of the Moon29.3 – 34.1arcminutes

What Does k = (1 + cos θ) / 2 Measure?

The illuminated fraction connects two quantities that describe the Moon's appearance from Earth: how much of the visible disc is lit (k), and the geometry that determines it (θ, the phase angle at the Moon between the Sun and Earth). Together they define every phase of the lunar month, from the first thin crescent after New Moon to the brilliant, fully illuminated disc of Full Moon, and back through the waning phases to the next New Moon.

The formula k = (1 + cos θ)/2 is a pure geometric identity. It requires no physics beyond the assumption that the Moon is a sphere illuminated by a distant Sun, and that the observer is far away compared to the Moon's size. Yet from this simple relationship emerges the entire monthly cycle that has structured human calendars for millennia, and that continues to drive everything from the timing of religious festivals to the planning of astronomical observing sessions.

The Illuminated Fraction Formula

The defining relationship is:

k = (1 + cos θ) / 2

where k is the illuminated fraction (0 to 1) and θ is the phase angle at the Moon in degrees, between the direction to the Sun and the direction to Earth. Rearranged to solve for θ:

θ = arccos(2k − 1)

Related quantities that follow from k and θ:

Illuminated percentage = 100 · k
Elongation (waxing): ψ = 180° − θ
Elongation (waning): ψ = 180° + θ
Lunar age = (ψ / 360°) · 29.53059 days

Equivalently, in terms of the illuminated percentage P (0 – 100%):

θ = arccos(2P/100 − 1)

Illuminated Fraction Variables

SymbolMeaningNotes
kIlluminated fractionFraction of the visible lunar disc that is lit; ranges 0 to 1
θPhase angleSun–Moon–Earth angle at the Moon; 0° = Full, 180° = New
ψElongationSun–Earth–Moon angle; ranges 0° to 360°, distinguishes waxing from waning
ageLunar ageDays since the most recent New Moon; 0 to 29.53
TSynodic month29.53059 days; the cycle length of the phases
PIlluminated percentage100·k; the form most commonly used in almanacs and apps

How Each Variable Affects the Appearance

k and θ are linked by a simple cosine, and the relationship is not linear. Near Full Moon (θ close to 0°) the illuminated fraction changes slowly — from θ = 0° to θ = 22.5°, k drops only from 1.000 to 0.962. Near the quarters the change is much faster — from θ = 67.5° to θ = 90°, k drops from 0.691 to 0.500, a fall of nearly 0.20 over the same angular interval. And near New Moon (θ close to 180°) it slows down again: from θ = 157.5° to θ = 180°, k drops only from 0.038 to 0.000.

This behaviour is a direct consequence of the derivative dk/dθ = −sin θ / 2, which vanishes at θ = 0° and θ = 180° and reaches its maximum magnitude at θ = 90°. Practical consequences abound: the Moon looks "full" to casual observers for three or four nights in a row, because k stays above 0.95 over that entire range. Meanwhile, the difference between a two-day-old crescent and a three-day-old crescent is very noticeable, because k is changing rapidly in that part of the cycle.

The wavelength-averaged brightness of the Moon as seen from Earth is approximately proportional to k, but with an important subtlety: the Moon's surface reflects light non-uniformly, so the illuminated disc looks brighter near the sub-solar point and dimmer near the terminator. Near Full Moon, this backscattering effect makes the Moon dramatically brighter than a simple k-linear model would suggest — a phenomenon known as the "opposition surge". The apparent magnitude of the Moon at Full is roughly −12.7, while at First Quarter it is only about −10.0 — a factor of 12 in brightness, even though k is only halved.

The illuminated fraction is also responsible for one of the most striking naked-eye features of the Moon: earthshine. When k is small — a thin crescent a day or two after New Moon — the dark side of the Moon is not truly black. It is faintly illuminated by sunlight reflected off Earth, a phenomenon described by Leonardo da Vinci in the 16th century. Earthshine is only visible near the crescent phases, because when the Moon is close to New as seen from Earth, Earth is close to Full as seen from the Moon, and so reflects its maximum possible light back onto the Moon's night side.

Illuminated Fraction Calculation Examples

Given: θ = 60° — solve for k
k = (1 + cos 60°) / 2 = (1 + 0.5000) / 2 = 0.7500 (75.00% illuminated)
Given: θ = 90° — First or Last Quarter
k = (1 + cos 90°) / 2 = (1 + 0) / 2 = 0.5000 (50.00%)
Given: θ = 120° — solve for k
k = (1 + cos 120°) / 2 = (1 − 0.5000) / 2 = 0.2500 (25.00%)
Given: k = 0.75 — solve for θ
θ = arccos(2 · 0.75 − 1) = arccos(0.5000) = 60.00°
Given: k = 0.25 — solve for θ
θ = arccos(2 · 0.25 − 1) = arccos(−0.5000) = 120.00°
Given: k = 0.75, waxing — full metric set
θ = 60.00°
ψ = 180° − 60° = 120°
Age = (120 / 360) · 29.53059 = 9.84 days
Phase: Waxing Gibbous
Given: k = 0.75, waning — same k, different phase
θ = 60.00° (unchanged)
ψ = 180° + 60° = 240°
Age = (240 / 360) · 29.53059 = 19.69 days
Phase: Waning Gibbous

Frequently Asked Questions

Because the geometry is a projection, not a linear measure. As the Moon moves through its orbit, we see the sunlit hemisphere from progressively different angles. When we look at it edge-on (quarter phase), the visible lit portion is exactly half the disc — but the Moon has already travelled a quarter of its orbit since New Moon. The relationship between the orbital angle and the visible illuminated area follows a cosine, which is why k = (1 + cos θ)/2 rather than a linear function. This is also why the Moon appears to change shape fastest near the quarters and slowest near Full and New.

Because the illuminated fraction k depends only on the magnitude of the phase angle θ, which is always between 0° and 180°, and it is the same whether the Moon is growing or shrinking. A 50% illuminated Moon occurs twice per month — once at First Quarter (waxing) and once at Last Quarter (waning). The two cases are geometrically mirror images: at First Quarter, the right side is lit (Northern Hemisphere); at Last Quarter, the left side is lit. The phase name, the lunar age, and the elongation all differ between the two, even though k and θ are identical. The toggle tells the calculator which side of the cycle you are on.

Because the "quarter" refers to the phase (one quarter of the synodic month has elapsed since New Moon), not to the illuminated fraction. At First Quarter, the Moon has completed roughly 7.4 days of its 29.5-day cycle — one quarter — but the visible disc is exactly half lit, since θ = 90° and k = 0.5. The naming is historical: the quarters of the lunar month are New, First Quarter, Full, and Last Quarter, and the phase names describe the cycle position rather than the appearance. In informal speech, "half moon" usually refers to a quarter-phase Moon, but the technically correct term is "quarter".

Not directly. The Moon is tidally locked to the Earth, so it always shows us the same face — the "near side". What changes is how much of that face is illuminated. At New Moon, the entire near side is dark (night on the Moon's near side), and we see no illuminated disc. But the far side — the "dark side" of popular song — is at that moment fully lit. The far side was not photographed until the Soviet Luna 3 probe in 1959 and not seen by human eyes until the Apollo 8 crew orbited the Moon in December 1968. "Dark side" is really a misnomer: the far side receives just as much sunlight as the near side, averaged over a lunar month; it is simply never visible from Earth.

Earthshine is the faint illumination of the Moon's night side by sunlight reflected off Earth. It is visible to the naked eye as a soft grey glow filling out the otherwise dark disc of a thin crescent Moon, and it was described by Leonardo da Vinci around 1510. It is strongest a day or two before and after New Moon, because at those times the Earth appears nearly "full" as seen from the Moon, and reflects its maximum light back onto the lunar night side. Through a small telescope, earthshine reveals the dark maria and even major craters that are otherwise invisible during the crescent phases.

Yes — the relation k = (1 + cos θ)/2 applies to any spherical body illuminated by a distant source and viewed from a distant observer. It gives the phase of Mercury and Venus as seen from Earth, the phases of Jupiter's Galilean moons as seen from Jupiter, and the phases of distant exoplanets as they orbit their host stars. The only difference is that for planets, the phase angle depends on both the planet's and Earth's orbital positions, so it varies over a synodic period rather than a synodic month. The formula itself is universal — a geometric consequence of shading a sphere with parallel light and projecting the result onto a plane.

Two reasons. First, the Moon's orbit is elliptical, so its distance from Earth varies by about 12% between perigee and apogee; the angular size changes, and the phase at a given orbital angle shifts slightly. Second, the terminator — the line between the lit and dark hemispheres — is not perfectly sharp on the actual Moon; it is softened by the roughness of the lunar surface, by the finite angular size of the Sun as seen from the Moon (about half a degree, the same as from Earth), and by the fact that we see more illuminated area on crater rims and mountain peaks near the terminator. These effects are small — typically a percent or two — but they mean that the formula gives a very close approximation rather than an exact prediction of the visual appearance.

Brightness is roughly proportional to k but with a strong non-linear enhancement near Full Moon, called the opposition surge. Approximate apparent magnitudes: Full Moon −12.7, Gibbous −11.5, First Quarter −10.0, Crescent −8.0, New Moon (dark) around +0 as seen from Earth's night side. The Full Moon is about 12 times brighter than a quarter Moon, even though k is only twice as large. The extra brightening comes from the backscattering of sunlight by the lunar regolith — when the Sun is directly behind the observer, fine dust grains reflect light more efficiently than at any other angle.

Calculating...

Variables

Symbol Quantity Unit
k Illuminated fraction
θ Phase angle deg

What it means

The illumination fraction k is the proportion of the Moon’s visible disk that is sunlit, ranging from 0 (new moon) to 1 (full moon). It depends on the phase angle θ, the angle between the Sun, Moon, and Earth. The formula is a good approximation for a spherical body. It is used in lunar studies, for predicting moonlight brightness, and in astrophotography to plan exposures. It also appears in calculations of tidal forces and in spacecraft navigation. Understanding this helps in observing the Moon and in interpreting light curves of variable objects.

Worked example

Moon Illumination Fraction – Two Detailed Examples

Real‑World
Scenario: An amateur astronomer is planning a night of deep‑sky imaging and wants to know how bright the Moon will be. The Moon's phase angle θ is 45° from the Sun (i.e., the angle between the Sun, Moon, and observer). They compute the illuminated fraction k = (1 + cos θ)/2. A value of 0.85 means about 85% of the lunar disk is illuminated, which will affect the background sky brightness and may require narrowband filters.
ParameterValue
θ (deg)45
1cos(45°) = 0.7071
2k = (1 + 0.7071)/2 = 0.8536
Result 0.854 (85.4%) ✓ Illuminated fraction
Scenario: A photographer wants to capture a crescent Moon. The phase angle θ is 135°, which corresponds to a thin crescent. They use the formula to predict that only about 14.6% of the Moon is illuminated, giving a beautiful thin crescent appearance. This helps them plan the optimal time for the photograph.
ParameterValue
θ135
1cos(135°) = -0.7071
2k = (1 - 0.7071)/2 = 0.1464
Result 0.146 (14.6%) ✓ Crescent Moon
Insight: The illuminated fraction k is a simple function of the phase angle. It ranges from 0 (new Moon) to 1 (full Moon).

Common mistakes

  • Illumination fraction: The fraction of the Moon’s disk that is illuminated as seen from Earth.
  • Phase angle θ: The angle between the Sun and the observer as seen from the Moon – ranges 0° to 180°.
  • k = 0: New Moon (θ=180°); k = 1: Full Moon (θ=0°).
  • First/Last quarter: θ = 90° → k = 0.5.
  • Assumption: Uniformly illuminated sphere – limb darkening is ignored.

Applications

Moon illumination fraction, k = (1 + cos θ)/2, where θ is the phase angle, gives the fraction of the Moon's disk illuminated as seen from Earth. This is used in lunar observations, photography, and for understanding tidal forces. Amateur astronomers and astrophotographers use it to plan imaging sessions – a full Moon (k=1) is bright, while crescent phases (k<0.5) show more surface detail through shadows. The illumination fraction also influences the brightness of the night sky, affecting deep‑sky observations. By calculating k, researchers can model lunar surface brightness and study the Moon's reflectance. This simple formula is a staple of lunar science and public outreach.

  • Lunar observation planning and imaging
  • Determination of lunar phase and visibility
  • Modelling of lunar surface brightness and thermal properties
  • Planning of astronomical observations to avoid moonlight
  • Educational astronomy and outreach

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  • Published July 10, 2026
  • Last updated August 18, 2026