METAR Code
FG
Weather Symbol
This type of fog forms when warm, moist air moves over a colder surface (such as land, water, or a surface covered by snow or ice) and cools to 100% humidity.
Associated terms coming soon:
Dewpoint, high-pressure system, inversion, and mesoscale are all terms associated with advection fog that will be coming soon to the Aviation Meteorology Reference.
Ingredients
In order for advection fog to form, warm, humid air is moved by the wind (i.e. advected) over a much cooler surface, such as a cold landmass or a body of water, as shown in this diagram of favorable ingredients. The warm air will be cooled from below by being in contact with the cold surface (AKA conductive cooling). This movement of warm air over a cool surface creates a stable layer (a surface inversion), and prevents surface air from mixing up into the atmosphere.
Structure
Advection fog forms (as shown in this image) when warm, moist air advects over a colder surface, causing the air in contact with the surface to cool by conduction. If the air mass at the surface is able to cool to the dew point temperature and reach 100% humidity (i.e. become saturated), there is a possibility that advection fog will form.
It is possible for fog to form before saturation occurs when the process is taking place over the ocean, due to the presence of abundant salt particles suspended in the air that can act as nuclei that are able to absorb and retain moisture. In the latter case, further cooling is required for low visibilities to occur.
Visibility typically drops rapidly as the air mass moves over a tight gradient in sea surface temperatures.
Land barriers/higher terrain along a coast may prevent fog from advecting inland, known as a wind barrier effect.
Duration
As long as favorable conditions persist, advection fog will remain and even continue to grow if the temperature contrast increases between the air and the colder surface, and additional moisture is added.
At night, the cooling of the land surface may allow fog to spread from the coast further inland. In this case, there are both radiative and advective processes at work.
Due to the broad nature of advection fog, it can persist for days on end, until there is a wind shift.
Image Source: Environment and Climate Change Canada
This image shows a simplified example of ideal conditions for fog development. Onshore flow ensures a constant source of moisture from ice-free, relatively warm (TW) bodies of water (oceans, lakes in fall, etc), over cold ground. A large difference in ground (TG) and air (Ta) temperatures make certain that air temperature can be cooled sufficiently to the dew point temperature (TD) of the incoming warm air, and saturate inland.
Critically, the cold surface temperature should be equal to or below the dew point temperature of the warm air mass, so that the warm air may be cooled from below to saturation. For example, if the dew point temperature is 10oC, and the cold surface is only 12oC, then the cold surface is not sufficiently cold to cool the warm air to saturation.
There are many situations where warm air is moved over colder surfaces, but the likelihood of fog development increases under a few ideal conditions:
It is also possible for cool air to move over warm water and create advection fog. This happens as moisture from the water will evaporate into the cold air, lifting the dew point temperature of the air to meet the air temperature.
Image Source: Environment and Climate Change Canada
Dissipation
This animation is an idealized visualization of diurnal behavior of advection fog through the day. As the sun rises, exposed Earth warms and causes the fog to gradually lift and clear over land, turning into stratus, and remaining as fog over waters. When the sun sets again, the surface cools, and onshore winds will push fog back on land.
This fog tends to drift onshore and may thin as the ground heats. If the land is warm due to limited diurnal heating, the air will mix and become turbulent. This turbulence combined with convective heat transfer between the air and the surface will dissipate fog, or cause it to lift and become stratus cloud, as shown in the animation below.
However, to dispel a region of advection fog, a change in air mass or wind direction is required to push the fog out. A new wind direction may bring drier and/or cooler air removing the two necessary ingredients of both moist and warm air. Alternatively, the change in wind direction may no longer push the warm moist air over the cold area anymore, but instead move it to a new location. If it is pushed to a location where the land is warmer than the air mass, fog will lift and dissipate.
An increase in wind strength can also help improve conditions, as it causes turbulent mixing within the cloud.
Image Source: Environment and Climate Change Canada
Advection fog prevails in the region where two ocean currents with different temperatures flow next to one another. Such is the case over the Atlantic Ocean off the coast of Newfoundland, where the cold southward-flowing Labrador Current lies almost parallel to the warm northward flowing Gulf Stream. When there is a high-pressure region located over the Atlantic Ocean, warm southerly air will move over the cold water and often produce fog in that region throughout the year and especially in summer.
This is an example of sea surface temperature gradients being caused by ocean currents. A ridge of high pressure over the ocean ensures southerly flow of warm air up the coast, bringing warm air across the sea-surface temperature gradient over cool waters in the north.
Image Source: NOAA
This image shows Canada's climatology from 1951-1980 of the average annual number of days with some fog. Examples of regions where advection fog tends to form in different seasons include:
As seen in the second image within the "Science Explained" carousel, coastal areas in Canada are more impacted by fog than landlocked areas due to advection fog forming in these regions, although it is not impossible for advection fog to occur over large lakes.
Image Source: Environment and Climate Change Canada
Determining the onset of advection fog. This type of fog can occur at any time of day as long as the conditions are favourable.
This is an animated gif of the satellite image over CYYT (St. John's, NL) on December 9, 2022 from 0400Z to 0700Z. The following colors are of importance in the animated gif: blue represents high cloud, orange indicates areas of fog and stratus, and green shows the bare land and ocean.
Image Source: Environment and Climate Change Canada
Shown here is the sea surface temperature (SST) chart on December 9, 2022 at 00Z. The SST associated with the Gulf Stream range from 18 to 24°C, whereas the cool Labrador Current ranges from 1 to 3°C. Putting it all together: the GFA suggests that warm, moist air is being transported northward over the St. John’s, NL airport (CYYT) in between a low-pressure region south of Nova Scotia and a high-pressure region northeast of Newfoundland. Satellite imagery and the METARs show that fog is advecting into CYYT in easterly flow.
Image Source: Environment and Climate Change Canada
Low visibility and/or ceilings yield various impacts depending on available aircraft and airport systems as well as crew certifications and capabilities. Loss of arrival or departure capabilities, loss of visual cues possible.
In CYYZ, we rely on the forecasts from our third-party weather forecast service provider and the TAF to indicate reduced visibility, especially if it is expected to drop below 1SM. We would also monitor the air and dew point temperatures as indicators of the possibility of fog.
Since forecasting fog can be difficult, response to fog events are more reactive than proactive (e.g. implementation of the Low Visibility Operations (LVOP). From a preparation perspective, review of LVOP standard operating procedures as well as ensuring the minimum equipment list (MEL) for the airfield are completed.
Because there are only three runways available for LVOP once RVR decreases to below 1,200ft (two arrival/departure runways – 05 and 06L – and one departure only – 33R), work on these three surfaces that could affect their availability for LVOP is scheduled outside the times of the year where there is a higher risk of fog. Otherwise, a way to recall the surface would be required so the impact to runway capacity is not so significant.
In CYVR, typically, we activate our LVOP when conditions are trending towards half of a statute mile but even prior to reaching those values ATC is likely to request that we set up for those operations on the airfield. This would mean restricting construction activities, removal of non-essential personnel from the airfield such as driver training, maintenance activities as required until the conditions improve.
We rely on the information disseminated from Environment Canada, the TAF and IBM Weather Forecasting contract services to indicate fog risks that could potentially impact airport operations. Our main objective is ensuring that we are prepared in case the fog materializes and this means the field lighting is inspected and ready to be available for LVOP.
Given our location, and coastal environment we tend to be prone to fog events which can contribute to increased costs:
Operations Duty Managers
Reductions in visibility can impact operations any time it deteriorates below 2SM. True impacts at an airport depend on the capabilities on the airfield specific to each runway, including the available instrumentation and lighting capabilities. Not all runways have the same capabilities, making it possible that the best runway for foggy conditions is not available because the prevailing wind is forcing operations on a different configuration. For example, in CYUL it is only 06L that has the best capabilities to operate in foggy conditions (CAT II operations). No other runway at the airport is certified to that same level, meaning that foggy conditions requiring CAT II or III (worse) while on a 24L/R or single runway 06R operation will lead to reductions in flow far more drastic than delays already felt if 06L was available. Of note specifically to forecasters: this specific caveat can change the landing/alternate limits based on which runway is active (among other factors specific to aircraft type/crew certification).
Because of the difficult nature of forecasting fog, additional weather forecast products can be referenced to determine its extent and severity. Wind direction off Lake Ontario with a close temp/dew point spread can be a key indicator along with conditions at Billy Bishop. Surrounding stations on a METAR tool can also be good indicators when coupled with webcams (Burlington, Billy Bishop, or Brampton).
ATC (Major Tower)
Fog impacts at major towers are dependent on multiple factors specific to aviation. These factors include airport equipment, reduced/low-visibility plans, runway lighting and certification, combined with airline-specific capabilities and crew training. The same visibility and ceiling may have two completely different resultant impacts at two different airports, depending on all the factors listed above. Fog events require some basic preparation.
Examples below are for CYUL:
ATC (Regional Tower)
Fog impacts at regional towers are dependent on multiple factors specific to aviation. These factors include airport equipment, reduced/low-visibility plans, runway lighting and certification, combined with airline-specific capabilities and crew training. The same visibility and ceiling may have two completely different resultant impacts at two different airports, depending on all the factors listed above.
At CYAM (Sault-Ste-Marie, ON) fog is major in the spring and fall. Reduced visibility requires extra caution moving vehicles and aircraft around the field. Because CYAM is surrounded by water on 3 sides we often get fog over half the field and not the other half. Poor weather observations and forecasting of fog can result in unplanned reductions in serviceability.
Fog, in Aviation, basically means a ground-based cloud layer which obstructs Visibility to ½ SM or less (METAR abbreviation FG).
Mist (METAR abbreviation BR) is the reporting term used to describe a ground-based cloud layer that obstructs visibility to greater than ½ SM, but less than 6 SM. A related data point here is dewpoint depression (or spread). A specialist monitors this information at a properly equipped Weather Observing Site and can in this way verify the obstruction to visibility as being mist, versus another hydro or lithometeor (drizzle/haze/smoke/dust, etc).
This is vitally important information, because the presence of mist or fog in sub-zero weather also infers icing, potentially adversely affecting all airframes and carburetor-equipped aircraft in the area.
Fog has another important impact on flight operations. Good visibility is essential to Visual Flight Rules Operations in general, and IFR Operations during the departure and arrival phases (and taxiing as well, under very low visibility). Anything which restricts visibility is going to be of interest to all pilots.
The formation of fog or mist can take several paths. The mechanism of formation can be roughly equated with the intensity and duration of the phenomenon at the observation point. Frontal or advection fog tends to be thicker in density and longer in duration (hours or even days), versus radiation fog, which forms “pools” in low open ground under clear skies and dissipates in minutes or hours once sunlight reaches the surface of the earth. Upslope fog can last as long as the wind and temperature/dewpoint spread support it.
FIC
These different characteristics will define how an FSS briefs a pilot of the threat – i.e. if there is some radiation fog at the destination airport giving IFR conditions at the time of departure, a Specialist may be able to tell the pilot that by the time they arrive overhead their destination, it will be CAVOK. If there is a warm front arriving over the destination, though, the duration and density of frontal fog make this a potential “showstopper” for VFR pilots and maybe even IFR flights. There are other variables which come into play, but these examples illustrate the main differences of interest to Aviation Support staff.
AAS
As mist/fog can often be affected by local effects, and minute shifts in wind and temperature, Advisory Specialists are always very attentive when BR/FG is occurring, especially when the temperature is near or below freezing.
Fog has a large impact on ATC operations. When visibility is extremely low and the corresponding RVR dips below company thresholds, aircraft cannot land at airports and must hold. This is not complex on its own, but the main issue that arises with fog and low visibility are that different airlines have different minimums for flying approaches. Sometimes within a company, one aircraft can land at an airport with low visibility while an identical aircraft cannot (depending on pilot qualifications.) This makes for difficult sessions for air traffic controllers as we need to question everyone on what their minimums are and then pass them in front or clear them out of the way for aircraft who can land. The lack of consistency and the unpredictability create very complex situations coupled with rapidly changing conditions on the ground. For example, Pilot A informs ATC that they require 2600 RVR and 1/2SM visibility and Pilot B needs 1400 RVR and 1/4SM visibility. The conditions on the ground are 2800 RVR, so both aircraft can land. Conditions then deteriorate and drop to 2000 RVR. Pilot A needs to be removed from the ATC sequence so pilot B can fly an approach.
Hourly observations are closely scrutinized with the temperature and dewpoint spread being a key dynamic, although onshore wind and visibility is also considered. Oftentimes a potential alternate will not be considered when the dewpoint depression is close as it can be an indication of unforecast fog. Forecaster notes can often help in cases like this but there are limited amounts of TAF’s that support this feature. In those cases dispatchers are likely to reach out to the CMAC forecaster to gain additional required insight on the forecast.
Other weather forecasting tools used:
Fog will present significant operational difficulties. Generally our biggest concern is fuel for holding, approaches, and alternate airport diversions. Different countries often have other criteria for takeoff and landing.
An observation from a Canadian Airline:
“A single diversion created by fog, can have a snowball effect where the aircraft that diverted is no longer able to operate its next flight and the airline must make changes to this aircraft routing as it did not arrive at its destination. Subsequently, the outbound flight will now be delayed. This or else the airline will have to ferry an aircraft with a new crew to operate the next flight out."
Operations in northern regions can be particularly challenging as weather observations, and terminal forecasts are not as available. Often times, webcams, pireps and local company staff are the only way to know whether fog is present.
Observation from a Northern operator:
“Fog is a major player in the Nunavik operation. With all airports located along the coast, fog banks will be present over the bay, close to the coast and any changes in the wind (direction and/or speed) could drastically change the weather. Ice and advection fog can be thick and have a serious impact on the operation. As there is no reliable forecast in this area, wind direction, spread between temperature and dew point, PIREP and strong knowledge of the region are our main tools to forecast how fog will affect our operation.”
VFR general aviation (GA) pilots can be significantly affected by fog given that it reduces visibility well below minimum legal limits, leading to delays and/or cancelled flights. Fog can be variable and unpredictable once it sets in and even if it appears to be dissipating, it can reoccur under certain conditions. It can also occur on a very small scale (example: a lake), which can have significant impacts for VFR float planes but due to how small the feature may be may not be captured in forecast products. For this reason, it is important to look at the factors contributing to the formation and predicted dissipation of fog, information that could be received from a FIC weather briefing. This is also where PIREPs become invaluable. Having information, especially in/over regions that do not have TAFs or observations, can provide pilots, forecasters, and FIC specialists with a better understanding of where this phenomenon is occurring.
TAF, GFA are often used to predict fog and to a GA pilot often flying away from larger airports, the GFA can sometimes be more helpful because it describes conditions over a larger area than the TAF might not account for, but which might still affect the airport or area you will fly in. Auto observations can help a lot, as well as webcams for these airports. In addition to predictions for fog directly, pilots should be aware of the conditions that can produce fog (Temperature/dewpoint spread, wind, temperature history, geography, etc) and to be on alert for those conditions, even when fog is not predicted.
Fog seriously impacts visibility, so little difference is made between PROB/TEMPO/FROM if using the TAF product alone, that is why a good GA pilot will consider the products and factors described above. For GA flights and flight training, fog can lead to flight cancellations (loss of income) or diversions (increase in operating costs).
Impacts also vary based on the type of fog and how well it can be forecast. Understanding the risks and the type of fog forecast (radiation fog, advection fog, frontal fog) becomes important to VFR pilots, from both a flight planning and safety perspective.