How to Calculate Sky Background Electrons
Convert sky surface brightness in mag/arcsec² to electron rate per pixel, aperture counts, and background noise.
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Required Calibration Convention
The zero point must be the magnitude corresponding to one electron per second. ESO documentation expresses the general photometric relationship as magnitude equals zero point minus 2.5 log10 of count rate.
Use the Sky Background Electron Rate Calculator with a sky brightness and zero point from the same filter and magnitude system.
Surface Brightness to Electron Rate
For sky surface brightness μ and electron-rate zero point ZP:
`rate per arcsec² = 10^((ZP - μ)/2.5)`
Convert to One Pixel
For square pixels with scale s arcsec/pixel:
`pixel area = s²`
`sky rate per pixel = rate per arcsec² × s²`
Exposure Stack
Sky electrons scale with rate, exposure time, aperture pixels, and exposure count.
Dark electrons scale the same way using dark current. Independent read-noise variance is read noise squared times aperture pixels times the number of reads.
Total Background Noise
For independent Poisson sky and dark signals plus Gaussian read noise:
`noise = sqrt(sky electrons + dark electrons + read-noise variance)`
ESO's exposure-time documentation uses the same structure for sky, read noise, and dark-current terms.
Important Calibration Checks
Confirm whether the supplied zero point is in electrons/second or ADU/second, whether extinction is included, and which aperture convention was used.
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Frequently Asked Questions
- Why does a darker sky have a larger magnitude number?
- The astronomical magnitude scale is inverse and logarithmic, so fainter surface brightness has a larger magnitude.
- Why does stacking add read-noise variance repeatedly?
- Each independently read exposure contributes another read-noise realization.
- Does this calculate source signal-to-noise?
- No. It calculates background terms only; source electrons and source shot noise must be added separately.
Last updated 7/20/2026