Warm season weather hazards
From hail and heat waves, to thunderstorms and tornadoes, severe weather in Canada takes many different forms during the warm months of the year, particularly the summer months.
Lightning is an electrical discharge caused by a buildup of static electricity between thunderclouds, or between thunderclouds and the ground. It can deliver as much as 100 million volts of electricity and strike a target up to 16 kilometres away, making it an extremely dangerous form of severe weather. When thunder roars, GO INDOORS.
Thunder is the noise created when air suddenly expands from the heat of a lightning discharge. If you count the seconds between a flash of lightning and a thunderclap, you can tell approximately how close the lightning is to you: each second representing about 300 metres. The Canadian Lightning Danger Map shows the movement of lightning strikes in real time.
Each year lightning kills approximately 10 Canadians and injures approximately 100 to 150 others. So, how do you keep yourself and your family safe when lightning strikes? The first and most important thing to remember is that if you can hear thunder, you are within striking distance of lightning. When thunder roars, GO INDOORS. If you cannot find a sturdy, fully enclosed building with wiring and plumbing, get into a metal-roofed vehicle. Stay inside for 30 minutes after the last rumble of thunder.
Once indoors, stay away from electrical appliances and equipment, doors, windows, fireplaces, and anything else that will conduct electricity, such as sinks, tubs and showers. Avoid using a telephone connected to a landline.
If you are in your car during lightning, do not park under tall objects that could fall, and do not get out if there are fallen power lines nearby.
If you are caught outside, do not stand near tall objects or anything made of metal, and avoid open water. Take shelter in a low-lying area.
If caught on the water in a small boat with no cabin during thunder and lightning, quickly get to shore. Boats with cabins offer a safer environment, but it is still not ideal.
Remember that there is no safe place outdoors during a thunderstorm. Once in a safe location, remain there for 30 minutes after the last rumble of thunder you hear before resuming your outdoor activities.
People who have been struck by lightning do not carry an electrical charge and can be safely handled. However, victims may be suffering from burns or shock and should receive medical attention immediately. If you come across someone who has been struck, call for medical assistance immediately. If breathing has stopped, administer mouth-to-mouth or cardio-pulmonary resuscitation (CPR).
Did you know
Both Ontario and the Prairies each experience on average about 20 short-lived severe thunderstorm rain events per year.
On August 19, 2005, up to 175 mm of rain fell over Toronto in less than 2 hours. Total costs from damage associated with the storm exceeded $500M - the second largest loss event in Canadian history.
In June 2010, multi-day rains in southeastern Alberta and southwestern Saskatchewan led to a washing out of the TransCanada Highway lasting for days and isolating many communities.
In Manitoba, late May 2010 saw 59 mm of rain at the Winnipeg Richardson International Airport but up to 108 mm in the southeast section of the city. Many basements were flooded and roads washed out. The Province of Manitoba issued overland flooding advisories.
Other severe rainfall events have occurred in Toronto in 2013, Calgary in 2013, and Ottawa in 2017, leading to damaging floods.
Due to the highly localized nature of heavy rains that arrive with some thunderstorms, some events are never recorded.
The provincial governments are responsible for issuing Flood Forecasts and Warnings.
Two types of summer heavy rains
- Large-scale weather systems with long-term rainfall: These large weather systems can last several days. Environment and Climate Change Canada issues Rainfall Warnings for this type of event.
- Short-lived thunderstorms with significant rainfall: Within a short period of time, sometimes only minutes, localized downpours from thunderstorms can produce flash flooding. Environment and Climate Change Canada issues Severe Thunderstorm Warnings for these types of rainfall events.
Heavy rain safety
Routinely monitor the Environment and Climate Change Canada weather forecasts for watches and warnings of potential heavy rains or severe thunderstorms with local heavy downpours. Know potential risks for flooding in your area and plan an escape route to higher ground. However, keep in mind that the threat of lightning is greater on high ground. During heavy rains, avoid roadway underpasses, drainage ditches, low-lying areas and water collection areas. They can unexpectedly flood or overflow. Do not try to drive on a flooded road. You cannot tell the condition of the road under the water.
Stay away from power lines or electrical wires during floods. Monitor the provincial government flood forecasts and warnings.
Localized, short term rain event. July 11, 2004. SW Edmonton
Large area, multi-day rain event. June 19, 2010. AB/SK border
Most flooding occurs when the volume of water in a river or stream exceeds the capacity of the channel. Flooding also takes place along lake and coastal shorelines, when higher than normal water levels inundate low-lying areas.
Numerous factors affect streamflow, and therefore the potential for flooding. Most important are the amount and type of precipitation, the nature and condition of the drainage basin, and climate.
Flooding is essential to a healthy environment, but can cause human hardship and economic loss.
Over the past 40 years, flood forecasting and warning in Canada has evolved into a network of forecast systems across the country.
A storm surge is an abnormal rise in water level where a high and forceful dome of wind-driven ocean water sweeps towards the coastline. This happens near where the eye of a tropical or non-tropical storm makes landfall, or passes close to the coast.
Often accompanied by high waves, storm surges can cross the normal high-water mark defined by the tide, and cause damage to infrastructure along coastal areas. They can also cause coastal flooding as far inland as several kilometres.
In the event of a storm surge, avoid coastal areas, particularly those prone to flooding, and seek higher ground.
Strong wind does not only occur on a large scale from tropical storms or low-pressure systems and fronts. It can also occur on a small scale from thunderstorms, Chinooks or the local geography.
Strong winds, and especially gusty winds, can cause property damage or turn any loose item into a dangerous projectile. They can also create unsafe travelling conditions that affect your ability to safely steer your car.
When there is a wind warning for your area, expect inland winds to be blowing steadily at 60-65 km/h or more, or winds that are gusting up to 90 km/h or more. Secure or put away loose objects such as outdoor furniture or garbage cans, put your car in the garage, and bring livestock to shelter.
High wind combined with heavy rain increases the risk of tree limbs breaking or trees uprooting. After heavy winds, check your property for dead branches and damage. With winds between 60 and 70 km/h, you will have difficulty with balance and walking against the wind. Twigs and small branches could also blow off trees and cause a hazard, so stay inside until it is safe.
Stay alert. The tendency is to hunch over and look down when facing strong wind. However, you may not see a wind projectile approaching. Listen for Environment and Climate Change Canada warnings of all types.
Watch for signs of wind in the sky. Swirls of dust on the ground or approaching waves on water, or shelf clouds beneath thunderstorms are often associated with strong gusty winds.
Seek shelter, preferably indoors away from outside walls, especially large glass surfaces. Avoid large open spans in buildings such as gymnasiums or malls.
Thunderstorm “straight-line” winds
Across much of Canada, “straight-line” winds, not tornadoes, cause most thunderstorm wind damage. Straight-line winds are winds that move horizontally along the ground away from thunderstorms, sometimes with tornado-like force. These strong winds may be technically labelled as microbursts, downbursts, squall lines, plough winds or derechos and may cause swirling dust and debris often confused with tornadoes.
Just like with tornadoes, straight-line winds can cause damage by blowing down trees or buildings. Roofing debris, tree branches, or unsecured construction materials blowing in a storm may become lethal projectiles and can cause significant damage if they hit something. Wind-driven rain or large hail may follow the strong winds and hide potentially dangerous or deadly flying debris. Straight-line winds may produce the same roar, like a freight train noise, often associated with tornadoes.
Did you know
The Environment and Climate Change Canada wind criteria for a Severe Thunderstorm Warning is wind gust speeds of 90 km/h or greater.
Straight-line winds can be as strong as some tornadoes but usually cover a much larger area.
Across the Prairies, there are on average 45 to 50 thunderstorm-related severe wind events that are not tornadoes. Ontario experiences approximately 40 to 70 severe wind events. Wind events are more common than tornadoes.
On July 23, 2012, a severe thunderstorm moved across Renfrew and Lanark Counties in eastern Ontario. Straight-line winds of up to 170 km/h downed many tens of thousands of trees, and knocked out power to over 25,000 customers, including the town of Calabogie.
On July 15, 2008, a severe thunderstorm brought straight-line winds to areas between Taber and Medicine Hat in Alberta. At some points along the path, the damage was 30 km wide with winds possibly in excess of 200 km/h.
An approaching shelf cloud, a sign that strong wind is imminent. The hanging tendrils may appear to be rotating and extending towards the ground, but are not usually associated with a tornado.
A tornado is a violently rotating column of air extending between a cloud base and the surface. When over water, a tornado is called a waterspout. While often depicted as a funnel with the narrow end on the bottom, there is no typical tornado. Tornadoes are highly variable in their appearance, strength, speed, direction of movement, and duration.
Most tornadoes develop in the late afternoon and early evening but may occur at other times, including overnight.
While wide, damaging, straight-line thunderstorm winds are often confused with tornadoes, tornadoes can produce some of the highest wind speeds on the planet. Most Canadian tornadoes have maximum wind speeds under 180 km/h, but can still cause serious damage. A small percentage can be considerably stronger with devastating impacts. Although Doppler radar is a major aid to weather forecasters to predict larger tornadoes, many smaller ones are very difficult to forecast.
Map of all verified tornadoes in Canada between 1980 and 2009, coloured by F-scale. From Sills, D. (Environment Canada) et. al (2012).
Map of Canada. Updated 30-yr tornado database including all confirmed and probable tornadoes between 1980 and 2009.
- Black circle: F5 category tornado, 1 recorded
- Red circle: F4 category tornado, 5 recorded
- Orange: circle: F3 category tornado, 24 recorded
- Green circle: F2 category tornado, 119 recorded
- Blue circle: F1 category tornado, 478 recorded
- Purple circle: F0 category tornado, 1217 recorded
Monitor Environment and Climate Change Canada watches and warnings and keep an eye on the sky - tornadoes can develop very rapidly.
When a tornado threatens, take shelter immediately, preferably in the lower level of a sturdy building. Mobile home residents should go to their shelter area . If caught outdoors with no shelter available, lie flat in a ditch, ravine or other low-lying area and shield your head with your arms.
Recent research has shown that tornado winds finding their way into a building through open doors and windows can lead to large internal pressures and greater damage. When a watch is issued , ensure that all doors and windows are closed. Flying glass and other debris pose the greatest danger to human safety.
Did you know
Each year on average, about 43 tornadoes occur across the Prairies and about 17 occur across Ontario and Quebec. The peak of the season is June through August.
Just as the Richter scale measures the intensity of earthquakes, the Fujita or F-scale measures the severity of an event by estimating the wind speed, whether tornadic or straight-line, based on the damage caused. The F-scale goes from weak F0 to incredible F5.
On April 1, 2013, Environment and Climate Change Canada began to use an improved version of the F-scale known as the Enhanced Fujita or EF-scale. While the levels of intensity, ranging from EF0 to EF5, have the same relationship to damage as the original F-scale, the associated wind speeds have been made more accurate. All events from April 2013 forward are rated using the EF-scale.
There is only one documented F5 in Canadian history, at Elie, MB June 22, 2007. Fortunately, there were no injuries, as the tornado was nearly stationary.
Three of the four deadliest tornadoes in Canada have occurred in the Prairies:
- Regina, Saskatchewan, June 30, 1912: F4, 28 fatalities in Regina, two more south of the City
- Edmonton, Alberta, July 31, 1987: F4, 27 fatalities
- Green Acres Campground, Pine Lake, Alberta, July 14, 2000: F3, 12 fatalities
The most deadly Ontario tornado was the June 17, 1946 Windsor F4 event , which caused 17 fatalities. The largest tornado outbreak in the province occurred on August 20, 2009, when 19 tornadoes developed over southern Ontario.
There is not a strong correlation between the physical size of a tornado and its maximum wind speed. All tornadoes, regardless of appearance, are potentially lethal threats.
A tornado usually moves along a narrow path from the southwest, west or northwest but may suddenly change direction. Groundspeed can vary from nearly stationary to 90 kilometres per hour, the path can be more than 20 km long and 400 m wide, and its duration can be up to one hour. In very rare events, tornadoes can be 1 to 2 kilometres wide and travel more than 100 kilometres.
If you see a tornado, and it does not appear to be moving, it is likely either moving straight away from you or straight towards you.
The roaring or freight train sound often attributed to tornadoes is not strictly a tornadic effect. The noise is caused by strong winds moving around and past obstacles such as trees and buildings. In open country, tornadoes may only emit a whine or whistle-like noise.
Hail forms when updrafts in thunderclouds carry raindrops upward into extremely cold areas of the atmosphere, where they freeze and merge into lumps of ice. When the lumps become too heavy for the updraft to support, they fall to the ground at speeds of up to 100 km/h or more.
Hailstones as large as grapefruit have been reported in Canada, but even smaller hail can be dangerous and can cause extensive damage in a matter of minutes.
The Prairies are especially vulnerable to hail. The Prairies receive more severe hail events and more damage to crops and personal property than from all other summer severe weather events combined, including tornadoes, severe thunderstorm winds and heavy rains. Ontario is the other hail-prone area of Canada with over one quarter of the summer severe weather events due to hail.
Partially melted hail stones. July 12, 2010 record Calgary hailstorm.
What a hailstone can do! August 3, 2009 Sundre, AB.
Routinely monitor the Environment and Climate Change Canada weather forecasts, watches and warnings for thunderstorms, which may include hail.
When hail or thunderstorms threaten, seek shelter in a solid building and stay away from windows, glass doors or skylights. If you are in a vehicle, find a place to safely pull off roadways and protect yourself from possible shattered glass. If caught outdoors and there is no available shelter, crouch down, face away from the wind and protect your head and neck with your hands.
Look out for flooded areas. Excessive hail, when combined with heavy rain, can plug storm drains and suddenly create local flooding. Remember the danger of lightning. When outside, stay away from tall objects such as large trees, towers, metal fences or poles.
Did you know
Severe Thunderstorm Warnings are issued for anticipated severe hail events. Severe Thunderstorm Warning criteria for hail is hail 20 millimetres in diameter or greater (nickel-sized or larger).
Canada’s “Hail Alley” resides in Alberta and is an area from just south of Calgary to just north of Red Deer and west of Highway #2 into the foothills.
On average, the Prairies receive approximately 130 severe hail events per year. Ontario receives between 25 and 30 severe hail events.
Two-thirds of Canada’s major documented hailstorms have occurred in Alberta*. Eight of Canada’s 18 largest hail insurance claims have involved the City of Calgary*. (*data courtesy of Public Safety Canada’s Canadian Disaster Database)
On average, July is the most active month of the year for hail. However, one of the costliest hailstorms in Canadian history occurred in Alberta in September .
Record-sized hailstones are named after the individual who finds and preserves them. The largest hailstone recorded in Canada was the Gawel stone (290 grams) near Cedoux, Saskatchewan in August 1973 (Charlton 1997, 1987 Edmonton Tornado Atlas, University of Alberta).
A thunderstorm on July 2, 2012 in northwestern Ontario produced extremely large hail in the Sioux Lookout area. One hailstone was measured with a diameter of about 9 centimetres - some of the largest hail the province has seen in years.
Heat and humidity
Humidity is the amount of water vapour in the air. High humidity makes people feel hotter than they would on a drier day. This is because the perspiration that cools us down cannot evaporate as quickly in moist, saturated air. To better describe how hot it feels in such circumstances, Canadian meteorologists developed the Humidex, a parameter that combines temperature and humidity in order to reflect the perceived temperature.
Relative humidity is the amount of moisture that the air contains compared to how much it could hold at a given temperature. In contrast, absolute humidity is the amount of moisture in a particular volume of air, measured in grams per cubic meter. A figure of 100 percent relative humidity would mean that the air is saturated. At this point, mist, fog, dew and precipitation are likely.
Relative humidity is normally at its maximum when the temperature is at its lowest point of the day, usually at dawn. Even though the absolute humidity may remain the same throughout the day, the changing temperature causes the ratio to fluctuate.
Heat and humidity safety
It is important to stay safe during such extreme temperatures. Avoid working or exercising intensely if it is very hot or humid outside, and head for cooler conditions if your body becomes overheated. If working outdoors is an absolute necessity, drink plenty of liquids and take frequent rest breaks. Be sure to maintain salt levels in your body and avoid high-protein foods . Also, ensure to protect pets from the heat and give them plenty of water to drink. Watch for signs of serious medical conditions, such as heat exhaustion and heat stroke.
The Humidex is a Canadian innovation that was first used in 1965. It describes how hot, humid weather feels to the average person. The Humidex combines the temperature and humidity into one number to reflect the perceived temperature. Because it takes into account the two most important factors that affect summer comfort, it can be a better measure of how stifling the air feels than either temperature or humidity alone.
The Humidex is widely used in Canada. However, extremely high readings are rare except in the southern regions of Ontario, Manitoba and Quebec, as well as southern sections of Alberta and Saskatchewan. Generally, the Humidex decreases as latitude increases. Of all Canadian cities, Carman, Manitoba, holds the highest recorded Humidex level at 53 on July 25, 2007. The hot, humid air masses which cause such uncomfortable weather usually originate in the Gulf of Mexico or the Caribbean.
Guide to summer comfort
Range of Humidex: degree of comfort
- 20 to 29: Little discomfort
- 30 to 39: Some discomfort
- 40 to 45: Great discomfort; avoid exertion
- Above 45: Dangerous; heat stroke possible
An extremely high Humidex reading is any reading over 40. In such conditions, you should reduce all unnecessary physical activity. If the reading is in the mid to high 30s, then you should tone down or modify certain types of outdoor exercise, depending on the individual age and health, physical shape, the type of clothes worn and other weather conditions.
If working outdoors is an absolute necessity, drink plenty of liquids and take frequent rest breaks. In hot, humid conditions, there is a considerable risk of heat stroke and sunstroke.
During the summer months, remember that animals also feel the heat. When the Humidex is high, take special care to ensure that your pet is well protected from the heat and has plenty of water to drink. Never leave pets or children in hot vehicles, even with the window down. On extremely hot days, the inside temperature of a car can be several degrees warmer than the air outside. It is therefore never safe to leave pets or children in a vehicle, even for a few minutes.
|Humidex||Degree of comfort|
|20 - 29||Little discomfort|
|30 - 39||Some discomfort|
|40 - 45||Great discomfort; avoid exertion|
|46 and over||Dangerous; possible heat stroke|
Humidex temperature and relative humidity
|Relative humidity (%)
Humidex for relative humidity from 60% to 20%
|Relative humidity (%)
Ultraviolet (UV) rays are the sun’s rays that can cause sunburn. Long-term exposure to UV rays is associated with skin aging, eye cataracts, weakening of the immune system, and skin cancer.
The amount of UV that you receive depends on both the strength of the sun's rays (measured by the UV index) and the amount of time you spend in the sun. The higher the UV Index number, the stronger the sun's rays, and the greater the need to take sun safety precautions. The UV Index is a 0 - 11+ scale .
Reduce your time in the sun, particularly between 11:00 a.m. and 4:00 p.m ., from April to September, and seek shade when outdoors. Cover up by wearing a broad-brimmed hat, a shirt with long sleeves, and wrap-around sunglasses. Use "broad spectrum" sunscreen with both UVA and UVB protection, with a sun protection factor (SPF) of 15 or higher.
Listen for Environment and Climate Change Canada's UV Index, which is included in your local weather forecast when it is forecast to reach 1 or higher (moderate) during the day.
Air Quality Health Index
The Air Quality Health Index measures the air quality in relation to your health on a scale from 1 to 10. The higher the number, the greater the health risk associated with the air quality. When the amount of air pollution is very high, the number measures as 10+. It provides local air quality forecasts for today and tomorrow with associated health advice.
You can refer to the Air Quality Health Index to check the quality of outdoor air in your community before heading off to work or play. You can also use its forecasts to plan your activities ahead of time.
Seniors, parents of children with asthma, and people suffering from diabetes, heart or lung disease, can use the index to assess the risk air pollution poses to their health and take steps to lessen that risk.
Fog consists of tiny water droplets suspended in the air that reduce visibility to less than one kilometre. It is different from cloud only because fog touches the earth’s surface.
Driving any vehicle in low visibilities due to fog can be hazardous and speeds should be reduced accordingly.
Frost is atmospheric moisture that crystallizes directly on the ground and on exposed objects, such as rooftops, when temperatures are below freezing. Frost forms under conditions that would normally create dew if the temperature were above freezing at the point of formation. Although it looks very pretty, frost can cause serious harm to flowers and plants if it occurs during the growing season. As such, take care to protect frost-sensitive plants when such conditions are forecast.
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