METAR Code
N/A
Weather Symbol
With the strong winds they produce, microbursts can produce a lot of damage over a relatively small area and in a short amount of time. Microbursts can produce wind damage comparable to that of a tornado, which is why they can also be rated on the EF-Scale. As they are capable of producing winds in excess of 160km/h, they are capable of uprooting trees, damaging infrastructure that is not well secured, and could even flip over smaller aircrafts.
The sudden change in wind speed and direction that a microburst produces is particularly hazardous, as it can cause sudden, severe turbulence.
Associated terms coming soon:
Low-pressure system and mesoscale are terms associated with microbursts that will be coming soon to the Aviation Meteorology Reference.
A microburst is a localized, powerful column of sinking air (downdraft/downburst) within a thunderstorm that is usually less than or equal to 4 km in diameter, which lasts for less than 5 minutes. With wind speeds that can exceed 160km/h, microbursts can cause extensive damage at the surface and pose a serious hazard to structures and aircraft.
Firstly, microbursts are meteorological phenomena associated with thunderstorms therefore, the main ingredients necessary for thunderstorm development must be present in order for a microburst to develop; moisture, instability, a trigger as well as wind shear are all essential for thunderstorm, and hence microburst, development.
There are certain features that forecasters look for in the environmental profiles that can promote the development of microbursts within thunderstorms. Any factor that increases the strength of the downdraft of a thunderstorm will enhance the potential for microburst formation. Some of those factors that forecasters look for in atmospheric profiles include:
Dry air aloft – Since dry air is more dense than humid air, it descends more easily than the moist air around it. So, as dry air mixes into a thunderstorm, it can enhance/accelerate the downdraft of the thunderstorm.
Strong winds within the dry mid-level layers – these stronger winds aloft create wind shear, which can also enhance the downdraft of a thunderstorm.
Cold air aloft – Similar to dry/moist air, colder air is more dense than warm air. When there is cold air aloft that can feed into the downdraft, the cold air can fall much more readily, and enhance the downward acceleration of the downdraft
Evaporative cooling – as raindrops within a thunderstorm reach the dry air aloft, some of them will evaporate. This evaporation causes the air to cool, which can contribute to the downward acceleration of the downdraft.
This is a diagram of a thunderstorm as well as the location of the microburst. The microburst occurs in the downdraft region of the thunderstorm. As the cold air descends rapidly towards the surface, it then spreads in all directions creating turbulence and extreme wind shear.
Image Source: NOAA
A process known as "downbursting" creates microbursts. Downbursts (also called downdrafts on a less intense scale) occur when a thunderstorm produces a column of cold air that is much denser than the surrounding air. This much higher density causes the column of air to descend rapidly towards the ground due to its greater weight, accelerating as it goes.
As the descending column of air reaches the ground, it spreads rapidly out in all directions. This spreading out of air at the surface is what defines a microburst. The strong outflow winds can be particularly dangerous because they can cause sudden changes in wind speed and direction.
This image is a zoomed in picture of the downdraft/downburst area of a thunderstorm. As the column of air descends rapidly towards the ground, it spreads out in all directions creating a rapid change in wind speed and direction.
There are two primary types of microbursts: wet microbursts and dry microbursts.
Wet microbursts are a type of microburst that involves a sudden and powerful downdraft of cool air from a thunderstorm which is accompanied by the presence of rain in the downdraft. As the downdraft that hits the ground and spreads out horizontally in a radial pattern. Wet microbursts can be spotted visually, as the precipitation falls rapidly compared to the rain around it.
Dry microbursts, on the other hand, do not contain precipitation. As the downdraft develops, the raindrops evaporate as the air descends to the surface resulting in a cloud-free column of air. Dry microbursts cannot be spotted visually unless their surface winds pick up dust or other particulate matter at the ground, since they are not associated with precipitation.
Image Source: WikipediaOpen a new window
Dissipation
Microbursts dissipate quickly, as the powerful downburst of cool air acts against thunderstorm development, since the spreading cold air at the surface can enter into the updraft region. However, microbursts outflow winds can act as a trigger for new thunderstorms that can develop new microbursts, since this cold outflow can collide with warm air near the system and force it aloft.
Duration
By definition, microbursts are a very short-term event. While conditions building to these intense events can last for several hours, the microburst itself typically lasts less than 5 minutes.
Microbursts can be difficult to forecast with much lead-time. As microbursts are associated with thunderstorms, this means that an accurate forecast for thunderstorm development is essential for the forecaster to determine whether these thunderstorms could produce microbursts. Thunderstorm forecast areas are typically refined 6-12 hours before thunderstorm development and are continuously updated as necessary.
An analysis of environmental profiles including the amount of moisture available to generate precipitation, mid-level winds and the presence of a dry layer in the mid-levels is key in determining whether a microburst could develop once thunderstorms have formed. Unfortunately, real atmospheric sounding data describing all of these features are only available at fixed times and locations, which do not always line up with thunderstorm development, so forecasters must rely on other data sources and model guidance to help their analyses.
There are many challenges in pinpointing exactly where a thunderstorm will develop within the forecasted area, thus forecasting an exact location for the development of a microburst particularly challenging, especially due to their inherently small nature.
Once thunderstorms have developed, forecasters typically use RADAR signatures to determine whether a microburst is occurring and can estimate the wind speed of the microburst.
GFAs do not specifically mention microbursts. Instead, their risk is captured within the thunderstorm (TSRA) and squall (SQ) group as their occurrence is directly tied to severe thunderstorm formation. Watches and warnings are issued by the Meteorological Service of Canada (MSC) when conditions exist and/or microbursts have been observed.
Similar to GFAs, TAFs do not specifically mention microbursts. The possibility of microburst development is included in the TSRA and SQ group with severity indicated by light (-), moderate (no prefix), or heavy (+) symbols. Watches and warnings for severe thunderstorms, including the possibility of microbursts, will be issued by the MSC when conditions supporting their development exist and/or microbursts are occurring. MSC also briefs commercial dispatchers and air traffic flow managers (NTMU, ACC Operations Duty Managers, etc.) on demand with respect to the risks associated with potential microbursts to help support critical decision-making and safe air traffic services delivery. This critical information is also passed along to pilots in preflight weather briefings from FIC specialists, and while in-flight whenever possible.
This is a sounding from a weather balloon launched at Amarillo Airport, Texas (KAMA) on July 22, 2011. Meteorologists only modified surface-level temperature and dewpoint to coincide with conditions expected just prior to the microburst occurrence. This was done to provide a clearer picture of the likely atmospheric profile and assess conditions that occurred that day in support of microburst formation.
Full detail behind the sounding is available on the NWS websiteOpen a new window. The presence of dry air close to the surface and the mid-levels combined with atmospheric instability supporting thunderstorm development with strong updrafts all played a role in the microburst that occurred that day in KAMA.
Image Source: National Weather Service
Discussions shown in this radar section will tie back specifically to radial velocities and diagnosing microbursts using this type of radar imagery. For those looking to get more background information, please visit this JetStream topicOpen a new window from the National Oceanic and Atmospheric Administration (NOAA).
The image on the left is the radial velocity snapshot from 2015Z on July 22, 2011. The yellow circle indicates the approximate location of KAMA airport. On the right is the actual location of the airport using the satellite overlay on the National Weather Service radar site. Due to its proximity, we can see that a large chunk of the northern side of the airfield is within what is known as the radar’s “Cone of Silence” (close-in area where data is unavailable due to the radar’s maximum tilt not allowing for scans to occur overhead).
Image Source: National Weather ServiceOpen a new window
These are two radial velocity snapshots taken at 2015Z (left) 2020Z (right). The arrow on the 2020Z image indicates the microburst captured by the radar with a peak velocity of 61KT. In the METAR tab we will see that the highest surface winds observed were 70KT gusts. For this snapshot, the peak velocity is a green “inbound velocity”, indicating that the radar targets were moving towards the radar just to the north of the microburst occurrence.
Radial velocities are critical in being able to assess microburst occurrences because they show meteorologists how radar targets are moving within and below a storm, something that is not possible solely with reflectivity or non-doppler radar. For more information, please visit this JetStream NOAA tutorial on how radars workOpen a new window.
Image Source: National Weather ServiceOpen a new window
This is a different example of microburst signatures, shown here because it provides a side-by-side screenshot of both the reflectivity (shown on the left, likely more familiar to most users), and the associated radial velocities shown on the right. The KLSX radar is shown at the center of the Cone of Silence (black circle). We can see the inbound velocities (green colors) closer to the radar and outbound velocities (brighter red colors, more evident in the northeastern cell) further away. The burgundy/gray line between the two (where the arrow points on the northeastern cell) is the centerline associated with the center of the microburst, where radial velocities are most likely to be perpendicular to the radar and therefore close or equal to 0.
Image Source: National Weather ServiceOpen a new window
Lastly, this is one final example of a microburst animation from the KIWA radar near Phoenix, AZ (date unknown). We can see the rapid outward spread of high velocities within minutes of the microburst occurring. The radar can be located off the left-hand side of the GIF. The bright green colors indicate radar returns moving toward the radar, while red indicates returns moving away from the radar, and the gray indicates movement exactly perpendicular to the radar. The rapidly increasing red and green velocities (indicating air that is spreading outward as opposed to air converging) is the location of the microburst.
Image source: Reddit/r/weather @Robot_templeton
These are the observations from KAMA from July 22, 2011. Notice the wind shift between 2024Z and 2029Z , and how they differ in both direction and strength as the microburst impacts the airfield. The radar is just to the north of the airport, and the strong green signatures on the radial velocities within the radar signature indicate strong winds towards the radar. This translates to the 70KT southerly wind gusts observed across the airport towards the radar just to its north. This event lasts only 12 minutes, with winds gradually diminishing afterwards. Lastly, a temperature drop from 38C at 1953Z to 23C at 2026Z was observed at the airport as a result of the cold air rushing down within the microburst.
Image Source: OGIMET
SIGMETs are not issued specifically for microbursts but will be issued for thunderstorms when criteria for transmission are reached or exceeded. It is important to note, however, that microbursts can occur within single storms that may or may not be within a SIGMET. As such, proper weather briefings and closely monitoring both forecast and actual conditions along with issued watches and warnings are imperative for this critically significant phenomenon.
Microbursts have led to deadly aviation disasters and pose a severe threat to aircraft. Windshear, loss/gain of speed, loss of control of the aircraft are all risks, and all in close proximity to the ground with little room available for recovery.
YVR
GTAA
Operations Duty Managers
There are no microburst-specific tools or technology available to diagnose potential occurrences at the airport. Impacts and planning here are the same as for thunderstorms.
ATC (Major and Regional Towers)
FIC
Microburst potential is greatest when there are thunderstorms with high bases, usually 6000ft AGL or higher, but these dangerous downdrafts can be formed by smaller Cumuliform clouds, too. When conditions exist that could allow microbursts to form, it is prudent for the Weather Observer to advise local ATC to be on the lookout for these anywhere around the airfield, with solicitation for PIREPS. Microbursts are particularly dangerous for Aircraft in critical phases of flight, such as during takeoff or landing. Enroute FISE positions can also assist pilots in maintaining situational awareness by requesting PIREPS on any Microburst observed inflight by VFR aircraft.
AAS
Advisory Specialists keep a keen eye out for signs of microburst activity when there is a risk they may be occurring. Be it watching the grass, trees, and windsocks for divergent wind directions, birds having difficulty staying aloft, dust clouds kicked up, etc. That said it is often very difficult to detect a microburst from visual sightings only. Aircraft will always be warned about the potential for Microbursts, and targeted PIREPs will be solicited.
This image is a representation of the Predictive Wind shear Display found on the A220.