Haze
Haze is a meteorological phenomenon caused by fine, dry particles suspended in the air, reducing visibility and giving the atmosphere a milky, faded appearance....
Fog is a dense suspension of water droplets or ice crystals near the ground that reduces visibility below 1 km, posing major hazards to aviation and transportation. Its types—such as radiation, advection, and freezing fog—are defined by international standards and require specialized operational responses.
Fog is a surface-based cloud consisting of minute water droplets or ice crystals suspended near the Earth’s surface, leading to a marked reduction in horizontal visibility—by international standard, to less than 1 kilometer. Fog is strictly defined in meteorology and aviation to distinguish it from similar phenomena such as mist or haze (which have less severe impacts or different causes). The presence of fog is a critical operational hazard, especially in aviation, ground transportation, and maritime navigation.
Fog forms when near-surface air becomes saturated, usually by cooling to its dew point or by the addition of moisture. Water vapor condenses onto microscopic aerosols (condensation nuclei), creating droplets typically between 1 and 10 micrometers in diameter. These droplets scatter light, causing the observed reduction in visibility.
Key factors in fog formation:
Fog’s persistence and dissipation are influenced by solar heating, wind mixing, and changes in humidity.
| Fog Type | Formation Mechanism | Typical Locations | Visibility Impact | Examples |
|---|---|---|---|---|
| Radiation Fog | Nighttime radiative cooling, calm winds | Valleys, lowlands | Severe | US Midwest, Oman highlands |
| Advection Fog | Warm, moist air over cold surface | Coasts, cold seas | Severe, widespread | San Francisco Bay, North Sea |
| Upslope Fog | Moist air forced upslope, cooling adiabatically | Windward mountain slopes | Moderate–Severe | Rockies, Oman’s Jebel Akhdar |
| Freezing Fog | Supercooled droplets at subzero temperatures | Cold regions, winter | Severe + icing | Alaska, Scandinavia |
| Evaporation Fog | Moisture added to cool air (steam, frontal) | Over water, post-rainfall | Localized | Sea smoke, autumn lakes |
| Hail Fog | Rapid cooling after hail accumulation | Patchy, post-storm | Localized, shallow | Midwest US |
| Ice Fog | Sublimation to ice crystals in extreme cold | Arctic/interior polar areas | Severe | Fairbanks, Alaska |
Note: Each fog type has unique operational and forecasting considerations, particularly for aviation and surface transport.
EGLL 250650Z 09004KT 0400 FG VV/// 01/01 Q1023 (FG = fog; visibility 400 m)Visibility thresholds:
| Code | Phenomenon | Definition/Remarks |
|---|---|---|
| FG | Fog | Visibility < 1 km due to water droplets |
| FZFG | Freezing fog | Fog with supercooled droplets, freezing on contact |
| BR | Mist | 1–5 km visibility, less dense than fog |
| HZ | Haze | Dry particles, not condensation-based |
Fog is a complex meteorological phenomenon with significant safety and operational implications. Its strict definition, classification, and international reporting standards are vital for mitigating risks in aviation, transportation, and infrastructure. Continuous advances in detection, forecasting, and operational response ensure that fog, while challenging, can be managed to minimize hazards and maintain safety in critical sectors.
According to the World Meteorological Organization (WMO) and International Civil Aviation Organization (ICAO), fog is defined as a suspension of water droplets or ice crystals in air near the surface, reducing horizontal visibility to less than 1 kilometer. This strict definition distinguishes fog from mist (1–5 km visibility) and haze (visibility reduction from dry particles).
The main types of fog include radiation fog (from nocturnal cooling), advection fog (from warm, moist air over a cold surface), upslope fog (air rising over terrain), freezing fog (supercooled droplets at subzero temperatures), evaporation/mixing fog (moisture added to cooler air), hail fog (rapid cooling after hail), and ice fog (ice crystals in extremely cold air). Each type is characterized by distinct meteorological mechanisms.
Fog is one of the leading causes of weather-related delays, diversions, and cancellations in aviation. It reduces runway and taxiway visibility, requiring the use of advanced landing systems, low-visibility procedures, and strict adherence to ICAO standards. Accurate measurement and reporting of fog (using codes such as FG and FZFG in METAR/TAF) are vital for safe airport and flight operations.
Fog is measured using visibility sensors such as transmissometers and forward scatter meters. At airports, visibility (in meters or statute miles) and runway visual range (RVR) are reported in METARs and TAFs using standardized codes: FG for fog, FZFG for freezing fog, with the threshold for fog set at visibility less than 1 km. Observations are made at least every 30 minutes or more frequently during changing conditions.
Operational protocols include the use of instrument landing systems (ILS) with varying categories (CAT I, II, III), enhanced runway and taxiway lighting, ground radar, and strict air traffic control procedures. Special weather reports (SPECI, SIGMET) are issued when fog is present or forecast to ensure flight crews and ground staff take appropriate safety measures.
Leverage advanced forecasting and visibility management to mitigate fog-related risks in aviation, transport, and infrastructure.
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