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Severe thunderstorms: your questions answered

Severe thunderstorms: your questions answered

All thunderstorms are pretty severe aren't they? Well no, only some are officially classified as 'severe'. So what exactly sets these storms apart and when are they most likely to happen? You asked and our meteorologists answered these—and lots more—of your storm questions.


What makes a thunderstorm 'severe'?

We see a lot of thunderstorms with rain, lightning and thunder, but a 'severe' thunderstorm is when we might start seeing those storms cause damage or impacts to people and infrastructure. We classify a thunderstorm as 'severe' if we expect or observe that the storm is producing any of:

  • 2 cm hail (about the size of a $2 coin) or larger, which can damage crops and property;
  • wind gusts over 90 km/h, which can blow branches off trees and cause damage;
  • heavy rainfall that could cause flash flooding, e.g. flooding roads or creeks; and/or
  • tornadoes.

It's these potentially damaging thunderstorms for which the Bureau issues Severe Thunderstorm Warnings.

When hail larger than 5 cm across is expected, we add the words 'giant hail' to our warning. National and international studies have shown that hail of that size increases associated damage by several orders of magnitude—mostly because roofing tiles start to break.

Why doesn't the Bureau warn for lightning?

Every thunderstorm has lightning. Some have more than others, which can make a thunderstorm appear significant or severe but if we warned for lightning would have to issue warnings for every single thunderstorm. While lightning can be dangerous if you're outdoors, our warnings focus on those storms that are more likely to cause damage or other impacts.

Learn more about lightning here.

What is a supercell?

Any thunderstorm requires three basic ingredients to form: moisture, a lifting mechanism, and instability in the atmosphere. Addition of a fourth ingredient—wind shear—can organise a thunderstorm into what's called a supercell. Wind shear is the increase in wind speed with height, and the change in wind direction as you move up through the atmosphere. This leads to tilting and rotation of the updraft in a thunderstorm, into a kind of sloping corkscrew structure. This 'organisation' means the cool downdraft is separated from the warm updraft, so you don’t see any of the interference between the two that weakens non-severe thunderstorms.

These organised thunderstorms can last many hours and travel long distances, potentially causing considerable damage. The deep rotating column of air, tilting away from the downdraft, is also what can form tornadoes beneath the storm—see below. So when the Bureau observes or forecasts conditions that support deep rotation and separation of up- and downdrafts in storms, we issue Severe Thunderstorm Warnings.

Non-supercell thunderstorms can also produce some of the dangerous effects listed above, such as damaging winds and flash flooding, albeit for shorter periods. Whenever such hazards are observed in a storm, we consider it 'severe' and issue warnings.

What causes storms to split?

Severe thunderstorms can 'split' due to the influence of strong vertical wind shear, which the change in speed and direction of the wind as you move from the ground/surface higher up into the atmosphere (see above). This can cause the top of the storm to move in one direction (with upper-level winds) while the base of the storm moves in another direction (with winds closer to the ground). A vertical pressure gradient is set up, causing a strong upward force within the storm. Either side of this upward force, two separate updrafts develop and move away from one another, becoming two separate storms.

Do we get tornadoes like in the USA?

Australia does see around 30–50 tornadoes per year, but most of them are in areas with very low population. If there's no-one around to see it, we don't get a report of a tornado. They can't be identified from satellite imagery, for example, as they're underneath clouds. Australia has had some very strong 'F4' (Fujita scale 4) tornadoes, for example in Queensland in the 1970s–80s and in Bucca, Queensland, in the early 1990s, and an F3 tornado in Mulwala, Victoria, in March 2013. The USA, due to different atmospheric conditions there, sees around 1200 tornadoes per year—of which one or two might be rated EF5 on the enhanced Fujita scale. There's also a much larger population there to photograph and report the tornadoes that do form.

Tornado formation

What turns a thunderstorm into a hailstorm?

In any type of thunderstorm, there is likely hail well above the ground (5–7 km up), but most of it melts as it falls and reaches the ground as rain. In a more 'organised' thunderstorm, stronger updrafts hold more rain and hail above the 'freezing level' (the height at which rain starts to freeze) for longer, allowing freezing rain to clump together into larger and larger hailstones. Read more in our Explainer: how hail forms.

Do we get hail in the tropics?

It is quite rare to hear reports of hail in Darwin, for example, and when it does occur it's very small. The freezing level is the height above which raindrops in a cloud start to freeze and form hail (see above). In southern Australia, that's usually around 3–4 km up. In the tropics it's around 5–6 km up, giving hail much more time and air to pass through before it reaches the ground, so it mostly melts and falls as rain.

Why do we see stronger thunderstorms further north in Australia?

Storms in the Northern Territory, Queensland and New South Wales have more moisture and instability to work with than storms that form further south. Instability is when a warm 'parcel' of air will rise into cooler air aloft and keep rising of its own accord. This is conducive to large, vertical, turbulent movement of air. This effect can be measured in terms of the difference in temperature between air near the surface and air in the upper atmosphere or as convective available potential energy (CAPE)—how much energy a 'parcel' of air has as it rises. In Victoria and Tasmania, CAPE values may be around 500–1000 J/kg some days. At the peak of thunderstorm season in southeast Queensland, CAPE values can be over 2000 J/kg; while around Darwin tropical thunderstorms can see CAPE values up to 5000 J/kg. More instability gives storms more energy to work with—letting them grow larger and produce more rain, bigger hail and stronger winds.

What time of year do we normally see the most severe thunderstorms in Australia?

The warmer months from September to March or April are the peak season for severe thunderstorms in Australia, due to the added warmth and moisture in the air. We can get severe thunderstorms in the cooler months, though, mostly connected to cold fronts that cross southern parts of Australia.

Average frequency of severe thunderstorms in Australia by month

Are thunderstorms in Australia becoming more severe or more frequent?

Consistent with global studies, an increase in the proportion of heavy rainfall has been detected over Australia. Since the 1970s, we've seen an increase in how much of Australia receives more than 90 per cent of its annual rainfall in the form of 'extreme rain days'—that is days in the top ten per cent of 24-hour rainfall totals. Read more on the Climate Change in Australia website.

Does the colour of storm clouds say anything about what type of storm it is?

The colours seen in thunderstorm clouds depend on the ice content in the clouds, but also on the angle of the sun and how the sunlight penetrates the storm. Storm clouds generally appear dark blue or black, but sometimes you can see brown, green or red tinges:

Clouds can appear brown before a storm, particularly in the interior of Australia, when the updraft has picked up a lot of dust from the ground. That dust or dirt in the air can provide the 'nuclei' onto which water vapour condenses to form cloud, raindrops and hailstones.

The reason some thunderstorms appear green is still the subject of debate, but it seems that the green component of sunlight is scattered preferentially in stronger thunderstorms that contain large amounts of hail and/or larger hailstones—and perhaps also water droplets. It’s widely believed, and supported by anecdotal evidence, that the eerie green glow requires the presence of hail in the storm—but that doesn’t necessarily mean the storm will deliver hail on the ground (see above).

Early and late in the day, the sun's rays have travelled through more atmosphere and had more of their blue and green wavelengths scattered before they reach clouds, so it's mostly orange and red light that reflects off clouds around sunset and sunrise.

Do fish really fall from the sky in some storms?

It can happen! When tornadoes in a thunderstorm form over water (known as a water spout) or briefly cross a pond or lake, they can pick up a lot of water—and along with it, some small marine life such as frogs and small fish. These can be carried for some distance in the storm, depending on the strength of the updrafts.

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