Visibility
Horizontal visibility distance
What is Visibility?
Technical detailsVisibility measures the horizontal distance at which objects can be clearly distinguished, ranging from under 100 meters in dense fog to 50+ kilometers in exceptionally clear conditions. Reduced visibility below 1000 meters creates atmospheric effects perfect for moody photography, moderate visibility of 10-20km suits general landscapes, while exceptional visibility above 30km enables telephoto work with distant mountains and ultra-clear astrophotography. Visibility depends on fog, haze, precipitation, dust, and humidity, making it a comprehensive clarity metric.
Templates using this field
Related rule templatesDramatic Seascapes
Dramatic coastal conditions for powerful seascape photography — waves, weather drama, and dynamic light
Clear Dark Skies
Moonless nights with crystal-clear skies for deep-sky photography
Storm Chaser
Dramatic storm conditions — from atmospheric builds to active thunderstorms
Golden Glow
Perfect warm portrait light during golden hour
Blue Hour
When city lights balance with the deep blue twilight sky
Fog Hunter
Thick, moody fog for atmospheric forest and landscape shots
Soft Light
Gentle, even lighting that flatters any landscape
Cloudscapes
Multi-layered dramatic clouds for striking sky photography
Mirror Lake
Perfectly calm water for flawless reflections
Golden Hour
That magical warm light just after sunrise or before sunset
Painted Sky
Golden hour clouds lit up in orange, pink and gold
Fire Sky
Those rare, intensely red and orange sunset skies
Photography tip
How to use this conditionReduced visibility (<5km) creates atmosphere. Clear visibility (>20km) for distant subjects.
Visibility in photography
In depthVisibility quantifies horizontal distance at which contrast and features remain distinguishable, measuring atmospheric clarity from dense fog under 50 meters to exceptional transparency exceeding 50 kilometers, fundamentally determining what photography subjects and techniques remain viable. Unlike simple fog presence/absence, visibility provides graduated clarity measurement revealing atmospheric conditions from impenetrable mist to crystalline transparency.
Dense fog with visibility below 100 meters creates completely obscured conditions where foreground elements disappear into white void within meters, producing minimalist, ethereal images where isolation and mystery dominate. Light fog or mist at 200-1000 meters visibility strikes the sweet spot for atmospheric landscape photography: enough clarity for foreground detail and compositional depth, sufficient obscuration for mood and layered fading into backgrounds, creating those coveted layered mountain ridges and fog-shrouded forests. Moderate visibility of 5-10km indicates hazy conditions common in humid climates and polluted areas, where distant features blur into atmospheric perspective, working well for shorter-range landscapes but frustrating telephoto mountain photography.
Good visibility of 15-25km represents clear conditions suitable for most photography, where mountains 20km distant render with adequate clarity and atmospheric perspective adds depth without excessive haze. Exceptional visibility above 30km occurs in dry climates, after precipitation has scrubbed air, and during high-pressure systems, enabling stunning telephoto compression shots of peaks 40-50km away and astrophotography where Milky Way structure appears crisp rather than haze-dulled. Visibility below 10km eliminates long-distance photography but enhances atmospheric perspective effects where layered ridges fade progressively into haze, creating classic mountain vista depth. PhotoWeather tracks visibility forecasts to alert photographers to fog and mist opportunities when visibility drops below 2km, clear air windows after frontal passage when visibility exceeds 30km, and optimal moderate visibility of 8-15km that balances clarity with atmospheric depth. Visibility changes dramatically throughout days: morning fog under 500m often lifts to 10-20km by midday as sun heats surface, while evening humidity may reduce afternoon clarity from 25km to 10km as moisture increases. Understanding visibility helps photographers choose appropriate focal lengths and subjects: reduced visibility demands wider angles capturing nearby subjects, while exceptional visibility enables extreme telephoto work previously impossible through haze.
Frequently asked questions
Common questionsWhat is Visibility?
Visibility measures the horizontal distance at which objects can be clearly distinguished, ranging from under 100 meters in dense fog to 50+ kilometers in exceptionally clear conditions. Reduced visibility below 1000 meters creates atmospheric effects perfect for moody photography, moderate visibility of 10-20km suits general landscapes, while exceptional visibility above 30km enables telephoto work with distant mountains and ultra-clear astrophotography. Visibility depends on fog, haze, precipitation, dust, and humidity, making it a comprehensive clarity metric.
How does Visibility affect photography?
Reduced visibility (<5km) creates atmosphere. Clear visibility (>20km) for distant subjects.
What values are typical for Visibility?
Visibility typically ranges from 0m to 100000m. PhotoWeather monitors these values to help you identify ideal conditions for your photography goals.
Typical values
Value rangeRelated fields
Similar weather conditionsAerosol 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.
Smoke AOD (550nm)
Smoke component of aerosol optical depth (black carbon + organic matter). Indicates wildfire smoke or urban pollution affecting air quality and visibility.
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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