METAR Code
TS
Weather Symbol
Thunderstorms can cause a suite of impacts including:
A storm with thunder and lightning that is typically accompanied by heavy rain, gusty winds, and sometimes hail.
Associated terms coming soon:
Dewpoint, inversion, lake breeze, low-pressure system, mesoscale, orographic lift, tornado, and upslope flow are all terms associated with thunderstorms that will be coming soon to the Aviation Meteorology Reference.
Thunderstorms require three main ingredients for formation: moisture, instability and a trigger. A fourth ingredient, wind shear, though not necessary for thunderstorm development determines the type of thunderstorms that will develop. Thunderstorms that develop in low or no wind shear environments tend to be non-severe whereas severe thunderstorms are more likely to develop when wind shear is present.
This image is a Venn diagram showing the necessary ingredients for thunderstorm development. Non severe thunderstorms can develop when the first three ingredients (instability, moisture and a trigger) are present. For severe thunderstorms to develop, wind shear is also necessary.
Moisture
Moisture is the main energy source for thunderstorm development. Warm, moist air is more buoyant and less dense than cooler, dryer air. As this air rises and condenses, thunderstorms can develop and the continuous supply of heat and humidity allows them to persist longer. Forecasters look for moisture in a variety of ways, including looking for high dew point temperatures, morning fog/dew, and onshore flow from water sources, among others.
Instability
Instability is the second ingredient necessary for thunderstorm formation. Instability allows for warm moist air to rise into the upper levels of the atmosphere. The more unstable the atmosphere is, the more momentum air will have as it rises vertically in the air, meaning the thunderstorms create a stronger updraft that will help fuel the thunderstorms. More detail on instability can be found under the term “atmospheric instability”. Instability is assessed through use of weather balloon data, as well as scientific reasoning.
Trigger
The third ingredient necessary for thunderstorm development is a trigger. A trigger initiates or “kicks off” the vertical motion of the air in the atmosphere and thunderstorms begin to develop. A front, trough, lake-breezes, topography, and even daytime heating from the sun can all act as triggers to initiate thunderstorm development. The type of trigger does have an effect on the type of thunderstorms that will develop. Fronts will activate thunderstorms and push them along in an organized line, whereas triggers like daytime heating generally create more disorganized, isolated storms.
Wind Shear
Wind shear, which is the change in wind speed and wind direction with height, is one of the main ingredients that determines what type of storms will form and how long they will last. Its main effect is to tilt and rotate the cloud in such a way that the updrafts, which feed the thunderstorm with heat and moisture, become separated from the downdrafts. This prolongs the lifespan of these systems, and allows them to develop and intensify into more complicated and powerful structures.
For more information on how shear impacts convective systems, please refer to The COMET Program’s course: MetEd / Principles of Convection III: Shear and Convective StormsOpen a new window.
Image Source: Environment and Climate Change Canada
This image presents the three stages of development of a thunderstorm. In the developing stage, warm moist air begins to rise and condense. This forms the updraft region of the thunderstorm. In the mature stage, water droplets begin to form, and some begin to fall back down to the ground dragging cooler air from the upper levels of the atmosphere back down to the surface. In the dissipating stage, the updraft region gets cut off and the downdraft takes over. With no more energy feeding into the thunderstorm, it soon dissipates.
There are two main regions of a thunderstorm – an updraft and a downdraft.
The updraft region is characterized by warm, moist air rising vertically and being ingested into the thunderstorm. Maintaining the updraft region is necessary for thunderstorms to continue, as it provides the “fuel” into the storm, which generates precipitation. If this source of energy gets cut off, the thunderstorms enter the dissipation phase and fizzle out.
The downdraft region, however, is characterized by cooler air that descends from the upper levels of the atmosphere back down to the surface, bringing gusty winds and precipitation. As the cold air falls to the surface, it spreads out on the ground generating a “cold pool” of air and extending away from the cell, also called a gust front. Once the downdraft region dominates in the thunderstorm life cycle, it will eventually cut off the energy supply of the updraft region and the thunderstorm will begin to dissipate. The downdraft can also be forceful enough to generate gusty winds at the surface with any kind of thunderstorm, but tend to be more severe in thunderstorms that form in a wind shear environment.
The mix of updrafts and downdrafts within the system are what leads to turbulence within convective clouds. The stronger the up and downdrafts are, the more intense the in-cloud turbulence will be.
Additionally, icing conditions are likely in convective clouds, generally in the top-few thousand feet. This is because warm air is pulled up higher into the atmosphere, lifting the freezing-level.
Image Source: National Severe Storms Laboratory (NSSLOpen a new window)
A single cell thunderstorm is one that has a single updraft and downdraft. They often occur in low/no wind shear environments, meaning their updraft and downdraft are not rotated away from each other, and are more or less vertically stacked and working against each other. They usually form due to daytime heating on a hot summer day, are short lived, lasting typically an hour or less due to the downdraft acting against the updraft once the storm matures. Single cell thunderstorms typically remain sub-severe and have a structure similar to the image shown here.
When single cell storms do occur in environments with wind shear, they will persist for up to an hour. The figure shown here depicts the idealized life cycle of a single cell storm. Initiation (left) stages are dominated by updrafts forming the convective cloud, lifting moisture through an unstable atmosphere as initiated by a trigger. The mature stage (center) occurs when the storm is precipitating, and the up and downdrafts coexist. Dissipation (right) begins when the warm air taken in by the updraft is cut off, and the system begins to degrade.
Image source: Penn State Department of Meteorology and Atmospheric ScienceOpen a new window
Multi-cell thunderstorms consist of many single-cell thunderstorms, each with their own updraft and downdraft structure that interact with each other to form new storms. They typically develop in environments where there is some wind shear (usually “speed shear”: a change in wind speed, but not direction, with height), which tilts the updraft and downdraft away from each other in each of the single cells. Multi-cell thunderstorms can last for many hours as the updrafts and downdrafts interact with each other in different stages of a thunderstorm life cycle to form new thunderstorms.
This is an example of a multi-cell thunderstorm. On the left, we can see towering cumulus forming, each with its own updraft and in a different stage of thunderstorm development. In the middle of the diagram, these storm cells have matured, and precipitation has begun to fall back to the surface creating a downdraft. On the right, these cells are in the dissipating stage and precipitation is no longer present.
Image source: NOAA/NWS
This image shows the main features of a supercell thunderstorm. A supercell thunderstorm is a type of severe thunderstorm that is characterized by its long-lasting and rotating updraft, which is called the mesocyclone. Supercells are usually the most dangerous type of thunderstorm, and they can produce a variety of severe weather events such as large hail, damaging winds, tornadoes, and flash floods.
Supercell thunderstorms form in highly unstable environments with fairly strong directional and speed wind shear. The increase in wind speed with height, in combination with wind veering (turning clockwise) with height produced a rotating updraft, which can lead to tornadoes. This shear environment also tilts the cumulonimbus cloud, maintaining separated up- and downdrafts, and prolonging the storm’s life.
Image source: NOAA/NWS
Mesoscale Convective System is an umbrella term for large (mesoscale) groups of thunderstorms acting together, with very long lifespans. These systems are made up of several single-, multi-, and/or supercells, and can cover hundreds of kilometers of space. They develop in sheared wind environments, which can extend the lifespan of these storms as high as 12 hours or more. Some convective systems which fall into this category are squall lines, derechos, and mesoscale convective complexes. To explore MCSs further, please refer to The COMET Program’s course: Severe Convection: Mesoscale Convective SystemsOpen a new window
Image Source: COMET
Dissipation
This image is an idealized example of the cold pool cutting off warm being fed into the system, leading to the dissipation stage of the storm. Thunderstorms will dissipate when their energy source is cut off from the system (removing moisture), or as they move into more dry and stable environments (removing instability). Additionally, and importantly, weakening or dissipation of the trigger can also dissipate thunderstorms depending on its support, or cease to produce new storms.
For example, single cell thunderstorms triggered by peak daytime heating hours will cease to develop in the evening hours once the sun isn’t as strong. They will also enter the mature and dissipation stages faster, once the downdraft caused by falling precipitation will overpower and eliminate the updraft feeding the cell.
Multi-cell thunderstorms will dissipate once the “cold pool” that develops under the storm expands out so much that it displaces the warm air moving into the updraft, cutting off the moisture supply into the system. At this point, the thunderstorm will enter the dissipation stage, and precipitate out its remaining water content. These storms will also stop developing when they enter a new environment that is drier and cooler (cutting off heat and moisture), or when they enter a region with inadequate low level wind shear to maintain separation of the up and downdrafts, which will start the dissipation phase.
The act of thunderstorms moving down a significant hill (such as the Niagara escarpment) can also extinguish or weaken thunderstorms, as this downslope motion tends to dry out conditions in the low levels, limiting the additional moisture available to be taken in to fuel thunderstorms.
Supercell thunderstorms and MCSs, due to their complex natures, are less likely to self-extinguish, and are more likely to begin dissipating when moving into a less hospitable environment. Moving into a region that is colder and drier, more stable, or one with no or weak wind shear, will cease development and allow the downdraft region to cut off the warm, moist energy sustaining the system.
Duration
Thunderstorms can last anywhere between 20 minutes to over 12 hours depending on the atmosphere, and type of thunderstorms that develop.
Single cell thunderstorms, as mentioned, are very short lived and only last up to an hour, as the downdraft eventually dominates and cuts off the updraft region. Multi-cell thunderstorms can last for hours, as the various updrafts and downdrafts interact with each other to initiate more thunderstorms, and can even evolve into a mesoscale convective system or squall line. Supercell thunderstorms can last on the order of hours as well, but eventually lose their supercell structure and either dissipate or merge/evolve into a mesoscale convective system that can persist even longer.
Image source: Penn State Department of Meteorology and Atmospheric ScienceOpen a new window
This image is a distribution of thunderstorm warnings sent in Canada from 2012-2021.
Thunderstorm season typically begins in late May in Canada with peak occurrence in July and ends in mid-September. Thunderstorms are common but less frequent in the spring and fall and are very rare during the months of December to March.
The distribution and frequency of thunderstorms in Canada varies by region. In eastern Canada, thunderstorms are most common in southern Ontario and southern Quebec in particular, but also in the Maritimes, with the peak occurring in July and August. In western Canada, thunderstorms are most frequent in the southern portion of the Prairie Provinces as well as in the foothills of Alberta during the summer months with the peak occurring in June and July. Thunderstorms decrease in frequency at higher latitudes, although they do occur in the Arctic.
Image Source: Steven Flisfeder, Senior Program Meteorologist, MSC
While assessing the presence of ingredients needed for thunderstorm development (moisture, instability, trigger and shear) over large regions is not always complicated (depending on the strength/abundance of the ingredients), determining the specifics of exactly where, when or the intensity of each individual storm remains challenging in an ever evolving atmosphere.
Large continuous regions of thunderstorms that are expected to develop on large triggers (fronts, along onshore flow boundaries, orographic lift, etc) are generally easier to forecast and are more readily resolved by numerical guidance. However, for situations where thunderstorms are expected to be smaller in scale, exact location and timing of thunderstorms can present a much bigger forecast challenge for meteorologists. An analogy often used is watching a pot of water boil; we know that eventually, the first bubble will rise to the surface of the pot of water, however we cannot predict exactly where in that pot of water that first bubble will form. Numerical guidance struggles more to adequately predict thunderstorms that are not tied to synoptic features.
When applied to forecasting, forecasters can assess all the ingredients necessary for thunderstorm development (moisture, instability, the trigger and wind shear) to a certain degree of accuracy and over a larger area. However, even slight changes in these factors can influence whether thunderstorms develop or not, and how strong they may become.
It is more difficult to predict where each individual thunderstorm will develop, however once thunderstorms evolve into a more organized system (such as an MCS or a squall line), it becomes easier to predict storm motion and where the system will track.
Lastly, while there are certain values in different situations that forecasters look for while assessing thunderstorm potential, the balance between moisture, instability and wind shear is complicated. While instability might be abundant, a lack of moisture will still prevent thunderstorm development, as could a lack of trigger. Different triggers will also cause thunderstorms to take different paths. Due to how vast the country is as well, forecasting cues that work well in some regions, may not work well in others.
The GFA33 clouds and weather panel valid at 0000Z on August 4, 2023 shows a cold front associated with a low over central Quebec sweeping across southeastern Ontario and southern Quebec. Significant atmospheric instability exists, setting the stage for convective activity with frequent towering cumulus forecast to 27,000FT and occasional thunderstorms to 37,000FT within the green hatched area. The GFA also mentions the risk of a tornado across southern Quebec and eastern Ontario. Overall, a thunderstorm risk exists across much of the GFA area, though outside of the influence of the low the risk is more isolated.
This TAF for Ottawa, ON (CYOW) is one of many examples of sites that saw thunderstorms forecasted on August 3rd and 4th. At CYOW, the forecaster isolated the most likely risk of thunderstorms and hail at the airport to between 2100Z August 3rd and 0000Z August 4th, coinciding with the passage of the cold front. The PROB40 indicates a higher confidence of the occurrence of thunderstorms, while TEMPOs are not usually added to the TAF until thunderstorms have already formed and can be timed to when they are expected to hit the TAF site using radar imagery.
The atmospheric profile for CYUL valid at 2300Z August 3rd is similar to many sites in the thunderstorm risk area that afternoon and represents the atmosphere pre-cold front. Warm surface temperatures, coupled with high surface dewpoints, an unstable vertical profile and a cold front as a trigger sets the stage for thunderstorm development.
Image Source: Pivotal Weather
The HRRR forecast model graphic for simulated RADAR reflectivity valid 2200Z August 3rd to 0600Z August 4th shows the main passage of the cold front across eastern Ontario and southern Quebec, with remnant thunderstorms still forecast to develop on its backside.
Image Source: College of DuPage
This is a snapshot from the previous GIF, valid at 2300Z August 3rd, shows the approximate location of the cold front serving as a trigger for thunderstorm development across the region.
Image Source: College of DuPage
The Traffic Flow Management Convective Forecast (TCF) chart, valid at 0100Z on August 4th, shows the areas of more organized convection across eastern Ontario and southern Quebec. The area with higher tops to 39,000 ft consists of storms forecast to fire along the cold front. This frontal passage adds to an already volatile environment and supports slightly higher tops when compared to storms forecast in the warm sectors ahead of the front.
Image Source: Aviation Weather Center
Multispectral GeoColorOpen a new window satellite imagery captured in one-minute intervals between 2230Z and 2330Z on August 3rd shows thunderstorm development across much of Ontario and Quebec, with storms along the cold front showing the greatest extent of coverage and size. At this time interval and resolution, it is also possible to see “overshooting topsOpen a new window” bubbling up in the strong updrafts within individual storms.
Image Source: CIRA
This is a snapshot of the satellite loop shown above that depicts the approximate location of the cold front at 2300Z. The front serves as the trigger for intense thunderstorms in an environment that already had all other thunderstorm ingredients (moisture instability and in this case wind shear) present.
Image Source: CIRA
RADAR imagery valid between 2300Z August 3rd and 0400Z August 4th shows thunderstorms tracking across eastern Ontario into the CYUL region.
Image Source: Environment and Climate Change Canada
METARs show the passage of thunderstorms over Ottawa, ON (CYOW) between 2137Z and 0100Z, with hail observed in SPECIs issued at 2224Z and 2228Z. This verifies the initial forecasts made in the GFA and TAF shown. A significant temperature drop from 25C to 18C is also noticeable as a result of the thunderstorm downdraft and associated cold pool. The temperature begins to rise once again following the passage of the thunderstorm. The gust front associated with the thunderstorm is also captured with wind gusts peaking at 36 KT at 2247Z.
Image Source: OGIMET
Severe/extreme turbulence, severe icing, loss/gain of speed, loss of lift, and all hazards from other potential weather phenomena occurring within thunderstorms (see associated terms).
YVR
GTAA
Generally, the following would be considered if there is forecast for thunderstorm:
Operations Duty Managers
Any size of a thunderstorm in proximity to an airport terminal along with duration can greatly impact operations depending on demand at that time.
This could necessitate TMI’s such as GS, GDP, MIT, holding at bedposts, halting ground operations due to nearby lightning and or wind shear/microbursts.
From a planning perspective, the following is most important to an operations duty manager at a major airport. It is two-tiered, with both the airport/terminal and the enroute taken into account:
Airport/Terminal:
Enroute:
Extent of coverage, timing, and trajectory of thunderstorms in the enroute
ATC (Major Tower)
ATC (Regional Tower)
Thunderstorms are relevant to our operation. If we notice them forecast on the TAF, or painting strikes on the RADAR we would inform VFR pilots who might be affected. Sudden changes in wind direction and speed also affect runway assignments. IFR Departures can also be affected if a cell(s) are located along the departure routes (SID), deviations may be requested and coordination is involved. TAF is the forecasting tool used, PROBs are taken into consideration from a planning or head’s up perspective but given demand controllers are more likely to respond to thunderstorms in the moment.
The type of Thunderstorm threat will be defined by the environmental factors which allow it to form, and these different situations demand slightly different approaches for Weather Briefers. An unstable airmass, such as found in a summer “Warm Sector”, may spawn individual thunderstorm cells. These are easy to see and avoid (unless already overhead). When conditions indicate that a cold front will pass through the warm sector, this demands a more pointed warning to aircrew, as it will be impossible to avoid the severe turbulence, precipitation and reduced visibility that is common to a solid line of thunderstorms. For Light Aircraft, this is a “showstopper”, whereas some Medium Aircraft can launch and climb prior to the arrival of the Cold Front.
Should conditions favour the development of a really big system, like a Mesoscale Convective Complex, you’ll see Dispatchers repositioning aircraft out of the path of the anticipated MCC path, with inbound and outbound flights rescheduled or cancelled outright.
So, one could say that the type and size of Thunderstorm elicits different proportional responses from FSS.
Specialists are often at the ready during potential convective development as visibility is often reduced due to haze on hot summer days, and the approach of developing convective clouds isn’t always obvious (the CI or AC visible above the Haze may not just be CI or AC). Thunderstorm passage is often a busy time for Weather Observers as special criteria are met in rapid succession as a Thunderstorm transits.
AAS
Advisory specialists watch for the tell-tale wind shift as the outflow boundary passes, sudden rapid fluctuations in air pressure and temperature, and sudden increases in visibility: all signs of an approaching/developing area of convective activity. Ground crews at airports will often coordinate with Advisory/Observation specialists to stay up to date on approaching hazards for personnel on the apron and manoeuvring areas. We often amend the advisory and determined runway to keep aircraft clear of approaching convective weather, as well as solicit PIREPs from anyone in the area to build a better picture of the convective activity for other aircraft, briefers, and forecasters.
Thunderstorms have a massive impact on our work as terminal controllers. While some pre-planning takes place, it’s much more adapting and reacting to what’s currently happening. We tend not to differentiate between thunderstorm types. However, as soon as thunderstorms are forecast in a TAF(even 30 percent), a few planning steps must be taken.
Below are all specifics from Montreal’s terminal ATC:
Usually, we’ll have one or two controllers working departures and one or two working arrivals. ATC work both arrivals and departures together in a small airspace. This is done safely in a highly procedural environment and mostly without coordination between terminal ATC as aircraft are on prescribed routes with little deviation. During thunderstorms, aircraft are more likely to deviate off their prescribed routing due to convection, at which point division of ATC responsibilities by task is no longer viable.
Thunderstorms create the most difficult work environments for ATC. We do not differentiate between different types of thunderstorms. We receive a weather briefing and are made aware that there could be thunderstorms that could cause delays and closures, but thunderstorms are generally a tactical event to be handled.
When a thunderstorm is passing over an airport, it can disrupt the airport to the point that arrivals and departures must pause (also referred to as ‘shut down the airport’ internally).
Controllers have a much lower aircraft capacity on their frequency during storms as each aircraft needs more time and attention. We are constantly gathering and passing information to and from pilots, managers, supervisors, and other controllers.
Important in the high level especially during the summer months. This phenomenon has a real impact on the operational level to such an extent that we will change our staffing. Due to the unpredictability of storm formation, movement and height we treat storms with a tactical mindset.
What’s important for us is to know what the tops of the cumulonimbus will be. Depending on the altitude the clouds reach, it could influence the deviations planes decide to take. Products such as CoSPA and TCF are used to determine echo tops and storm motion.
Thunderstorms increase workload as flights require updated information on thunderstorms and active SIGMETS. A risk of thunderstorms will drive conversations around pre-planning routes (SWAP) that avoid active areas of thunderstorms.
Thunderstorms are an important consideration for Dispatchers and Airline operations as they can cause significant disruptions to routine operations. While individual or isolated thunderstorms may move through a busy airport for a short period of time, delays associated with those initial flight interruptions can ripple through an airlines schedule for the next 24-48 hrs.
Thunderstorms can disrupt airline operations by:
Thunderstorms can lead to increase in cost:
Increased hazards:
Thunderstorm forecast impacts:
The general “Dispatch” classification of thunderstorms:
As thunderstorms can have significant impacts, there is an effort to validate forecasting by consulting multiple products to ensure consensus prior to making schedule adjustments. There are many weather forecasting products/tools that DX’s use to anticipate thunderstorms that vary from organization to organization however the most used are:
TAF- the primary means for forecasting TS at an airport.
TCF
CIWS/CoSPA is heavily relied upon for current and potential weather 8 hours into the future.
Additional Products:
Thunderstorms have a significant effect on flight safety in all phases of flight. Typical resources for thunderstorm forecasts are NAV CANADA and the Aviation Weather Service department of the NOAA.
If delays are expected we work with our dispatchers to plan fuel, alternates, and routing. This generally occurs approximately 1 to 1 ½ hours prior to departure. PROB30’s/40’s/Tempo etc will dictate our landing limits at the aerodrome.
Image Source: Twitter
General Aviation (GA) pilots are taught to be very cautious about TS, both directly and indirectly. We all know not to fly into them, but also not near them, or under them, especially in smaller GA planes, due to the surrounding potential effects – turbulence, precipitation, updrafts, and downdrafts.
Thunderstorms are to be avoided at all costs. The combination of low cloud, heavy winds and rain can severely damage a GA float plane and potentially leave a crew stranded. GFAs and FIC weather briefings are most useful to pilots who are not flying to/from aerodromes providing TAFs. Examples include float plane pilots and pilots flying to private airfields.
When planning a flight, thunderstorm possibility will usually be easy to identify, but the degree to which they will be present, as well as the various types of thunderstorms, can make for a challenging decision-making process.
When relying on forecast products, the GFA is useful to see the bigger picture of what regions are likely to contain storm activity, but they usually refer to the conditions of an air mass over a very broad area. Unless associated with a specific phenomenon such as a cold front, it can be hard to predict exactly where they occur, so a good pilot will read the GFA and create a plan of action with contingencies assuming that there is a possibility of isolated or scattered storms in the region they plan to fly.
If a TAF is available, the more predictable the occurrence, the easier it is to plan accordingly.
When available, radar observations are a very important and often underused tool that can show the size, speed and severity of a larger storm system.
In summer when there are chances of less predictable thunderstorms not related to a cold front or squall, pop up storms tend to keep everyone on higher alert in terms of go/no go decisions to fly. During all flight phases, good pilots who have assessed the risks and decided to fly will be constantly looking around to monitor changes in the weather activity in all quadrants surrounding them.
Flying directly beneath or in close proximity to a thunderstorm should never be attempted. This might be obvious when there is precipitation below the thunderstorm due to reduced visibility and it would be automatically avoided by a VFR pilot. However, during developing or dissipating stages, precipitation may not be visible and extra caution must be taken due to updraft or downdrafts that may be present and creating extra risk. Updrafts may be hard to counter and poor corrective action may cause pilots to enter a dangerous or excessive dive. A failure to react to an updraft could push the aircraft closer to cloud and potentially cause the pilot to enter IMC, which could have severe consequences for an untrained and/or panicking pilot. A downdraft could be difficult or impossible to overcome if the aircraft’s vertical climb speed is less than the speed of the downdraft, causing it to approach the ground. Incorrectly adjusting for the downdraft could result in a dangerously low airspeed and/or aerodynamic stall.