Smoke AOD (550nm)
Smoke component of aerosol optical depth (black carbon + organic matter). Indicates wildfire smoke or urban pollution affecting air quality and visibility.
What is Smoke AOD (550nm)?
Technical detailsSmoke Aerosol Optical Depth measures the combined contribution of black carbon (soot) and organic matter particles from biomass burning, wildfire smoke, and fossil fuel combustion to atmospheric opacity. These fine particles, typically smaller than 1 micrometer, are highly efficient at scattering and absorbing light, making even modest smoke concentrations devastating for photography. Smoke particles create neutral-to-cool-toned haze with characteristic grey, brown, or bluish coloration depending on composition and illumination angle, dramatically reducing contrast and color saturation while often producing eerily diffused or orange-red sunlight during heavy smoke events. Smoke AOD above 0.10 severely compromises landscape and astrophotography, though values of 0.20-0.50 during sunrise/sunset can occasionally create surreal red/orange sun disks for creative compositions. PhotoWeather's smoke forecasts help photographers avoid wildfire smoke plumes and urban pollution episodes.
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Related rule templatesPhotography tip
How to use this conditionSmoke creates grey/brown haze and dramatically reduces visibility. High smoke (>0.1) ruins landscape photography but can create dramatic diffused light effects. Check smoke levels for astrophotography.
Smoke AOD (550nm) in photography
In depthSmoke Aerosol Optical Depth (Smoke AOD) quantifies atmospheric light extinction caused by carbonaceous aerosols from biomass burning, wildfires, agricultural fires, and anthropogenic combustion sources, providing photographers with critical advance warning of visibility degradation from smoke plumes. This metric specifically tracks fine-mode aerosols (particle diameter less than 1 micrometer) composed of black carbon (elemental carbon soot) and organic carbon compounds produced during incomplete combustion. Unlike coarse mineral dust which produces warm-toned haze, smoke particles exhibit neutral to brownish-grey coloration with distinctive optical characteristics: strong light absorption by black carbon combined with scattering by organic carbon creates thick, opaque atmospheric haze that severely reduces visibility and photographic quality even at moderate concentrations.
Smoke AOD values below 0.03 indicate clean air with negligible smoke impact, 0.03-0.08 produces light smoke haze noticeable as slightly reduced clarity and muted colors but often still acceptable for photography, 0.08-0.20 creates obvious smoke haze with significantly degraded visibility and washed-out colors making most landscape photography challenging, 0.20-0.50 indicates dense smoke reducing visibility to a few kilometers with heavily muted colors and milky-white or grey-brown skies, while values exceeding 0.50 represent extreme smoke events (major wildfire plumes, severe agricultural burning episodes) that create apocalyptic orange/red lighting conditions with near-zero visibility for anything beyond close subjects. Wildfire smoke is the primary driver of high Smoke AOD in most regions: during active fire seasons (summer-autumn in North America, dry seasons in Australia, Southeast Asian burning season February-April), smoke plumes can travel thousands of kilometers from source fires, affecting photography across entire continents. The 2023 Canadian wildfire season, for example, produced Smoke AOD values exceeding 1.0 across the U.S. Northeast, creating orange skies and rendering outdoor photography nearly impossible for weeks.
PhotoWeather's integration of CAMS smoke forecasts helps photographers anticipate and avoid smoke plumes by providing 5-day predictions of Smoke AOD at your specific location. For astrophotographers, Smoke AOD below 0.05 is essential to avoid significant light extinction; for landscape photographers, values below 0.08 maintain acceptable clarity while values above 0.15 generally make high-quality work impossible. Some photographers embrace moderate smoke (0.15-0.30) during sunrise/sunset for dramatic red/orange sun disks and apocalyptic moods, though such conditions remain controversial and uncomfortable to work in.
Frequently asked questions
Common questionsWhat is Smoke AOD (550nm)?
Smoke Aerosol Optical Depth measures the combined contribution of black carbon (soot) and organic matter particles from biomass burning, wildfire smoke, and fossil fuel combustion to atmospheric opacity. These fine particles, typically smaller than 1 micrometer, are highly efficient at scattering and absorbing light, making even modest smoke concentrations devastating for photography. Smoke particles create neutral-to-cool-toned haze with characteristic grey, brown, or bluish coloration depending on composition and illumination angle, dramatically reducing contrast and color saturation while often producing eerily diffused or orange-red sunlight during heavy smoke events. Smoke AOD above 0.10 severely compromises landscape and astrophotography, though values of 0.20-0.50 during sunrise/sunset can occasionally create surreal red/orange sun disks for creative compositions. PhotoWeather's smoke forecasts help photographers avoid wildfire smoke plumes and urban pollution episodes.
How does Smoke AOD (550nm) affect photography?
Smoke creates grey/brown haze and dramatically reduces visibility. High smoke (>0.1) ruins landscape photography but can create dramatic diffused light effects. Check smoke levels for astrophotography.
What values are typical for Smoke AOD (550nm)?
Smoke AOD (550nm) typically ranges from 0.0dimensionless to 3.0dimensionless. PhotoWeather monitors these values to help you identify ideal conditions for your photography goals.
Typical values
Value rangeRelated fields
Similar weather conditionsVisibility
Horizontal visibility distance
Aerosol Optical Depth (550nm)
Total aerosol optical depth at 550nm. Lower values indicate clearer skies and more vivid colours.
Dust AOD (550nm)
Dust component of aerosol optical depth. High dust reduces air clarity and can create warm-toned haze.
Sea Salt AOD (550nm)
Sea salt component of aerosol optical depth. Indicates marine aerosols from ocean spray, common in coastal areas.
Ångström Exponent
Ångström exponent (α) computed from AOD at 550nm and 865nm. Indicates aerosol particle size: higher values = smaller particles (pollution, smoke), lower values = larger particles (dust, sea salt).
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