What If? Lab
What if lightning never struck?
Lightning is a giant spark in the sky. It even helps plants and some forests! What if there were no lightning? Let's imagine it with Olly.
Lightning is a giant electric spark from a storm cloud. It's powerful, but it also does useful jobs: it turns some nitrogen in the air into plant food, and its fires help some forests renew. Imagine a world where lightning never struck, and see what would change and what would carry on.
Lightning discharges charge separated inside thunderclouds, heating its channel to about 30,000 °C. Besides thunder, it fixes a little atmospheric nitrogen and ignites fires that some ecosystems are adapted to. This thought experiment removes it and weighs how much each role depends on lightning alone.
The big question
Flash! Lightning lights up a stormy sky. Then comes the rumble of thunder.
What if lightning never happened? Would we miss it?
Lightning is one of nature's most dazzling sights: a giant spark that lights up a storm cloud. The National Weather Service says lightning strikes the United States about 25 million times a year.
It can be dangerous, so the safety rule is simple: when thunder roars, go indoors. But lightning also does some surprising jobs in nature. So what would happen if it never struck at all? This thought experiment follows three ideas: plant food, forests and thunder.
Lightning is an electrical discharge that temporarily equalizes charge regions in a thunderstorm. About 25 million flashes reach the United States each year (NWS), and most flashes overall stay inside clouds.
This thought experiment asks which natural processes depend on lightning. Facts come from NOAA, the National Park Service and Nature Education; consequences are reasoned ideas. The safety message stays the same throughout: when thunder roars, go indoors.
Explore the idea
Make a prediction
If lightning never happened, what else would disappear?
If lightning never struck, which of these would disappear too?
Which phenomenon depends entirely on lightning?
- Thunder
- Rain
- Wind
-
Established fact
Lightning makes thunder and helps make some plant food.
Lightning causes thunder and fixes some nitrogen from the air into a form plants can use.
Lightning produces thunder and contributes abiotic nitrogen fixation, a minor share beside microbial fixation (NOAA, Nature Education).
-
An idea scientists discuss
A world without lightning is pretend. We imagine it carefully.
Lightning won't really stop. What would happen without it is an idea built from what lightning does.
Every consequence here is reasoned from lightning's known roles, not observed.
-
Established fact
Most lightning stays inside the cloud.
About 75 to 80 percent of lightning flashes stay inside the storm cloud and never reach the ground.
Because the in-cloud electric field is far stronger than the cloud-to-ground field, about 75–80 percent of lightning is intra-cloud (NOAA).
-
Established fact
When thunder roars, go indoors!
There is no safe place outside during a thunderstorm. When thunder roars, go indoors, into a building or a hard-topped car.
NWS: if you hear thunder you are likely within striking distance; substantial buildings and hard-topped vehicles are safe options.
-
Established fact
Plants can't use nitrogen straight from the air.
Nitrogen gas makes up nearly 80 percent of the air, but plants and animals can't use it until it's changed into another form.
N₂ is nearly 80 percent of the atmosphere but is unusable until fixed into biologically available forms (Nature Education).
-
Established fact
Tiny bacteria make most plant nitrogen. Lightning makes some.
Most nitrogen fixation is done by bacteria, but some nitrogen is fixed by lightning.
Most fixation is carried out by prokaryotes; some is fixed abiotically by lightning or industrial processes (Nature Education).
-
An idea scientists discuss
Plants would still grow, with help from bacteria.
Without lightning, plants would still get most of their nitrogen from bacteria, though some places might get a little less.
Losing lightning would remove one natural source of fixed nitrogen; the size of the effect would vary and is not estimated here.
-
Established fact
Some pine cones open in the heat of a fire.
Lodgepole pine cones open with the heat of a fire and drop their seeds onto freshly cleared ground.
Lodgepoles are adapted to their fire regime: serotinous cones open with heat, seeding the cleared ground (NPS Grand Teton).
-
Established fact
Park experts use some fires to keep forests healthy.
Fire managers at Grand Teton National Park use planned fires and some lightning-started fires to support fire's natural role.
Grand Teton managers use prescribed and lightning-ignited fires to restore fire regimes, and reduce fuels around communities (NPS).
-
An idea scientists discuss
Forests might change without lightning.
Without lightning, some fire-adapted forests might change, unless people planned fires to take its place.
Removing a natural ignition source would alter fire regimes; prescribed fire could partly substitute.
-
Established fact
Thunder is the sound of air heated by lightning.
Lightning heats the air to about 30,000 °C in a fraction of a second. The air expands so fast that it makes a shock wave: thunder.
Thunder is the acoustic shock wave from explosive expansion of air heated to as much as 30,000 °C (54,000 °F) (NOAA).
-
Established fact
Count after the flash to tell how far away the storm is.
Light travels much faster than sound. Count the seconds from flash to thunder and divide by 3 to get the distance in kilometers.
Sound travels about a third of a kilometer per second, so seconds ÷ 3 gives kilometers to the flash (NOAA NSSL).
-
An idea scientists discuss
Without thunder, we'd need other storm warnings.
Without thunder, people would rely more on weather forecasts and alerts to know a storm is near.
Thunder is a natural warning; without lightning there would be no such hazard, but also no such cue.
In our world
Inside a storm cloud, tiny bits of ice bump together. They build up electricity.
When there is enough, zap! Lightning jumps to balance it out.
Inside a thunderstorm, bits of ice and small hail bump past each other as air carries them up and down. The bumping separates electric charges: the bottom of the cloud usually becomes negative and the top positive.
Air doesn't let electricity flow easily, so a huge amount of charge builds up first. When there's enough, the air gives way and lightning flashes. NOAA says most lightning, about 75 to 80 percent, never leaves the cloud. Only some flashes reach the ground.
NOAA notes that exactly how lightning forms is still debated, but leading theories involve charge separation by collisions between ice, graupel and supercooled droplets, producing a negative cloud base and positive top. Air is a good insulator, so the field must grow strong before breakdown.
Because the field inside the storm is much stronger than that between cloud and ground, roughly 75–80 percent of lightning occurs within the cloud. The discharge heats its channel to as much as 30,000 °C (54,000 °F).
Switch the sparks off
In our pretend world, storm clouds still bring rain.
But there are no flashes and no thunder. What else would change?
In our pretend world, storms still form and rain still falls, but the charge in clouds never jumps as lightning. No flashes, no strikes, no thunder.
Follow the paths in the lab: food for plants from the air, forests that renew after fire, and a quiet sky with no thunder. Some of lightning's jobs might be done in other ways, and some might change a lot. Each card says whether it's a fact or an idea.
Assume thunderstorms still develop and precipitate, but breakdown never occurs. That removes lightning's nitrogen fixation, lightning-ignited fires and thunder at once.
The interesting question is substitution: nitrogen is mostly fixed by microbes, and fire can have other causes, so the consequences differ in size. These are reasoned ideas; the premise itself is not physically realistic.
Why lightning matters
Air is full of nitrogen. Plants need nitrogen, but they can't use it straight from the air.
Lightning's huge energy changes a little of it into a kind plants can use.
Nitrogen makes up nearly 80 percent of the air, and every living thing needs it. But plants can't use nitrogen gas as it is. It first has to be changed into another form, which is called nitrogen fixation. The two nitrogen atoms in the gas are held together very tightly, so breaking them apart takes a lot of energy.
Lightning has that energy, so it fixes some nitrogen. But most nitrogen fixation is done by tiny living things called bacteria, including bacteria that live in bumps on the roots of plants like peas and clover.
N₂ is very stable because of its triple bond, so converting it into biologically available forms, nitrogen fixation, needs a great deal of energy. Nature Education explains that most fixation is carried out by prokaryotes, some free-living and some symbiotic, such as Rhizobium in legume root nodules, while some nitrogen is fixed abiotically by lightning or by industrial processes including fossil-fuel combustion.
So lightning is one supplier among several. Without it, microbial fixation would continue, though some ecosystems might receive less fixed nitrogen from the air.
Lightning and forests
Some forests grow back after a fire. Some pine cones only open in the heat!
Park rangers know that fire can help those forests make room for new trees.
The U.S. National Park Service explains that fire is an important natural part of many forests. In Grand Teton National Park, lodgepole pines have cones that open with the heat of a fire, dropping seeds onto freshly cleared ground. Aspen and other plants there are boosted by fire too, and wildlife from elk to grizzly bears benefits from the fresh growth.
Today, park fire managers use carefully planned fires and some lightning-started fires to keep forests healthy. This careful work is done by trained fire crews.
NPS Grand Teton describes fire as an important natural disturbance. Each ecosystem has a fire regime: ponderosa pine forests have frequent, low-intensity fires, while Greater Yellowstone's lodgepole and mixed conifer forests burn every 100–300 years in large fires. Lodgepole serotinous cones open with heat, seeding the cleared ground.
Fire was feared and suppressed for much of the 20th century; today managers use prescribed and lightning-ignited fires to restore natural fire regimes, while reducing fuels around communities.
Amazing facts
-
Lightning is hotter than the outside of the Sun!
Lightning can heat the air to about 30,000 °C (54,000 °F), five times hotter than the surface of the Sun.
NOAA gives lightning channel temperatures of up to 30,000 °C (54,000 °F), about five times the Sun's surface temperature.
-
You can count to tell how far away a storm is.
Count the seconds between the flash and the thunder, then divide by 3. That's roughly how many kilometers away the lightning was.
Light arrives almost instantly and sound travels about 1/3 km per second, so seconds ÷ 3 ≈ kilometers, or ÷ 5 for miles (NOAA NSSL).
-
Scientists are still learning how lightning starts.
Even today, scientists still debate exactly how storm clouds build up their electric charges.
NOAA notes that exactly how lightning forms has never been verified; leading theories involve ice and graupel collisions.
Words to know
- lightning
- a giant electric spark from a storm cloud
- thunder
- the boom made when lightning heats the air very quickly
- nitrogen
- a gas that makes up most of the air; living things need it
- nitrogen fixation
- changing nitrogen gas into a form plants can use
- fire regime
- the usual pattern of how often and how strongly fires happen in a place
Discovery challenge
-
What should you do when you hear thunder?
What is the safety rule when you hear thunder?
The NWS lightning safety slogan is…
- When thunder roars, go indoors
- Stand under a tall tree
- Go swimming
Show the answer
When thunder roars, go indoors
Go inside a building or a hard-topped car.
Go indoors: a building or hard-topped car is safe.
'When Thunder Roars, Go Indoors!'
-
Who makes most of the nitrogen plants can use?
What does most of the nitrogen fixation on Earth?
Most natural nitrogen fixation is carried out by…
- Tiny bacteria
- Lightning
- Rainbows
Show the answer
Tiny bacteria
Tiny bacteria do most of it. Lightning helps a little.
Bacteria; lightning fixes some too.
…prokaryotes; lightning contributes an abiotic share.
-
What makes thunder?
What causes the sound of thunder?
Thunder is…
- Lightning heating the air very fast
- Clouds bumping together
- Rain hitting the ground
Show the answer
Lightning heating the air very fast
Lightning heats the air so fast that it booms.
Air heated by lightning expands explosively.
…a shock wave from explosive expansion of lightning-heated air.
-
Where does most lightning happen?
Where does most lightning happen?
About 75–80 percent of lightning is…
- Inside the cloud
- Between cloud and ground
- Under the sea
Show the answer
Inside the cloud
Inside the cloud!
Most stays inside the storm cloud.
…intra-cloud.
Experiments to try
- Watch What If? Lab What if rainbows appeared at night? A rainbow appears when light shines into drops of water from behind you. Sunlight usually does the job, but bright moonlight can too, making a faint “moonbow”. Explore moonbows, why the light must be behind you, and the ghostly white fog bow.
- Watch What If? Lab What if the wind stopped blowing? Wind is air rushing from places of high pressure to places of low pressure. It carries heat, water and weather around the world, lifts seeds to new homes and has pushed sailing ships across oceans. Imagine all the air going still, and follow what might change.
- Watch What If? Lab What if a forest grew back after a fire? In 1988, fires passed through about a third of Yellowstone National Park. Today, the young trees that sprouted afterward have grown into new forests. Follow the forest's comeback: the first plants, the pine cones that open with heat, and the animals that return.
Explore next
- Watch What If? Lab What if rainbows appeared at night? A rainbow appears when light shines into drops of water from behind you. Sunlight usually does the job, but bright moonlight can too, making a faint “moonbow”. Explore moonbows, why the light must be behind you, and the ghostly white fog bow.
- Watch What If? Lab What if the wind stopped blowing? Wind is air rushing from places of high pressure to places of low pressure. It carries heat, water and weather around the world, lifts seeds to new homes and has pushed sailing ships across oceans. Imagine all the air going still, and follow what might change.
- Watch What If? Lab What if a forest grew back after a fire? In 1988, fires passed through about a third of Yellowstone National Park. Today, the young trees that sprouted afterward have grown into new forests. Follow the forest's comeback: the first plants, the pine cones that open with heat, and the animals that return.
- Watch Try it What If? Lab What if Earth had no atmosphere? Earth's air works like a jacket: it keeps heat in and carries it around. Take the air away in our model of a sandy patch of ground on the equator, and the coldest part of the night drops from about 13 °C to about 2 °C.
- Watch Try it What If? Lab What if there were no greenhouse gases? Greenhouse gases such as carbon dioxide and water vapor hold some of Earth's heat in, like a blanket. Take them all away in our energy-balance model and Earth's average temperature falls from about 15 °C to about −19 °C, well below freezing.
- Watch Try it What If? Lab What if there were more greenhouse gases? Adding greenhouse gases makes it harder for Earth's heat to escape, so the planet warms until it balances again. In our model a small change in how freely heat escapes warms Earth by about 2.6 °C, and the oceans make the warming take years.
- Watch Try it What If? Lab What if Earth were covered in ice? White ice bounces sunlight back to space, so an icy planet soaks up less of the Sun's warmth. In our energy-balance model, making Earth reflect 60 percent of its sunlight instead of 30 percent drops its average temperature from about 15 °C to about −23 °C.
- Watch Try it What If? Lab What if glaciers melted? Glaciers are huge, slow-moving masses of ice on land. When land ice melts, its water runs into the ocean and raises the sea. In our model, melting every mountain glacier on Earth would lift the sea by about 40 centimeters; scientists' best estimate is a little less, about 32.
For parents & teachers
What children will learn
- Lightning is an electric discharge from charge built up in storm clouds.
- Thunder is the sound of air heated very quickly by lightning.
- Lightning fixes some nitrogen, but bacteria do most nitrogen fixation.
- Some forests are adapted to fire, and lightning is one natural source of it.
- Safety: when thunder roars, go indoors.
Recommended ages: 7 to 17 ยท About 15 minutes
Talk about it
- Which of lightning's jobs could something else do, and which could not?
- Why might park experts sometimes let a fire burn or plan one on purpose?
- How would you know a storm was coming if there were no thunder?
Try at home or in class
- From indoors during a storm, count the seconds between a flash and its thunder and divide by 3 to estimate the distance in kilometers.
- Make a tiny static spark: in a dark room, shuffle in socks on a carpet and touch a metal doorknob. That's a very small cousin of lightning.
Key vocabulary: lightning, thunder, nitrogen, nitrogen fixation, fire regime
Where these facts come from
- How Lightning Is Created (JetStream) , NOAA National Weather Service
- The Sound of Thunder (JetStream) , NOAA National Weather Service
- Severe Weather 101: Lightning Basics , NOAA National Severe Storms Laboratory
- Lightning Safety Tips and Resources , National Weather Service
- Lightning Safety Overview , National Weather Service
- The Nitrogen Cycle: Processes, Players, and Human Impact , Nature Education (Scitable)
- Fire Ecology (Grand Teton National Park) , U.S. National Park Service
Checked, not yet human-reviewed. Last updated October 26, 2026. Spotted a mistake? Tell us.