Tools

Airmass Calculator

What This Calculator Tells You

Airmass measures how much atmosphere light from a celestial object must pass through to reach you. At the zenith (directly overhead), airmass is 1.0. Near the horizon, light travels through much more atmosphere, increasing airmass and degrading image quality.

Calculator

The angle above the horizon (0° = horizon, 90° = zenith/overhead).

1.41
Very Good

Low airmass with minor atmospheric effects. Excellent for most observations.

Light Loss

~0.28 mag

Approximate extinction in visual band (assumes 0.2 mag/airmass)

Path Length

1.41x

Light travels 1.4x farther through atmosphere than at zenith

Common Airmass Values

AltitudeAirmassQuality
90°1.00Zenith
60°1.15Excellent
45°1.41Very Good
30°1.99Good
20°2.90Fair
10°5.59Poor
5°10.31Poor

Why Airmass Matters

Light Loss (Extinction)

More atmosphere means more absorption and scattering. Objects appear dimmer near the horizon - typically 0.2-0.3 magnitudes lost per airmass.

Atmospheric Dispersion

At high airmass, different wavelengths refract differently, creating color fringing. Planets may show red and blue edges.

Seeing Degradation

More atmosphere means more turbulence to pass through. Images become blurrier and less stable at low altitudes.

Astrophotography

Imagers often limit observations to airmass <2.0 (altitude >30°) for quality data. Airmass <1.5 is preferred.

Rules of Thumb

  • Airmass 1.0 = perfect: Only achievable for objects at the zenith
  • Airmass <1.5: Preferred for imaging and critical observation
  • Airmass <2.0: Acceptable for most purposes (altitude >30°)
  • Airmass >3.0: Generally avoid - wait for object to rise
  • The "30° rule": Serious observers often don't observe below 30° altitude

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