Storm science
Rare tornado types
Not all tornadoes look the same. Some spin backwards. Some come in pairs. Some cycle for hours. Here are the rare types.
Anticyclonic tornadoes
- Rotate clockwise (opposite of standard Northern Hemisphere).
- Rare: <1% of tornadoes.
- Form on LEFT flank of supercells (left-movers).
- Or in special storm modes.
- Wind physics identical to cyclonic; direction differs.
- Documented anticyclonic tornado: 2013 El Reno had one.
Satellite tornadoes
Independent tornado outside the main mesocyclone.
- Same parent supercell.
- Not a subvortex of the parent tornado.
- Rare but documented in famous outbreaks.
- Sometimes visible in wide chase shots.
- 2011 Tuscaloosa-Birmingham had documented satellites.
- 2013 El Reno โ chased alongside main.
- Distinct funnel from parent tornado.
Twin tornadoes
Two independent tornadoes
From same supercell but distinct.
1965 Palm Sunday
Multiple documented pairs.
2014 Pilger NE
Twin EF4s photographed and filmed.
2004 Roanoke IL
Filmed twin tornado.
2010 Wray CO
Photogenic twin landspouts.
Sometimes called
"Sisters" or "dyads" historically.
Multi-vortex tornadoes
One tornado containing multiple smaller vortices rotating around center.
- 2013 El Reno โ massive multi-vortex.
- 1999 Bridge Creek-Moore F5 โ visible subvortex structure.
- 2007 Greensburg EF5 โ filmed multi-vortex phase.
- Damage patterns highly variable in path.
- Peak winds in subvortices, not overall parent.
Cyclic tornadoes
Supercells that produce multiple tornadoes sequentially.
- Each tornado occludes and dies.
- New tornado forms east or northeast of previous.
- Can produce 4-8 tornadoes over hours.
- 1965 Palm Sunday outbreaks had cyclic supercells.
- 2011 Tuscaloosa supercell was cyclic.
- 2013 Moore day's parent storm was cyclic.
Wedge tornadoes
- Wider than tall.
- Not a distinct "type" โ a shape.
- Typically EF2+.
- Photogenic and terrifying.
- Sometimes multi-vortex under wedge shroud.
- 1990 Plainfield, 1999 Bridge Creek-Moore, 2013 Moore all wedges.
Rope tornadoes
- Thin, snake-like.
- Often end-of-life dissipation.
- Sometimes newly formed.
- Can still be EF3 despite thin appearance.
- Photogenic during rope-out.
- Beautiful photograph subject at sunset.
Cone tornadoes
- Classic funnel shape.
- The image most people picture.
- Common configuration.
- Range EF0-EF5.
- Most textbook images.
Stovepipe tornadoes
- Tall, narrow, straight column.
- Between rope and cone in width.
- Often EF2-EF3.
- Chaser-favorite for photography.
- Steady, well-defined.
Waterspout tornadoes (over land)
- Waterspouts that move onshore.
- Retain waterspout characteristics (not supercell-derived).
- Weaker typically.
- Rare in most regions.
- Common in Florida.
- Damage: weak-to-moderate.
Fire tornadoes
- Wildfire-generated true tornadoes.
- Extremely rare.
- 2003 Canberra Australia โ first officially documented.
- 2018 Carr Fire CA โ first EF-rated in US.
- Physics: pyroCB supercells.
- Increasing with fire season intensification.
Steam tornadoes
- Cold air over warm water in fall/winter.
- Very rare.
- Over Great Lakes occasionally.
- Photogenic.
- Weak vortices.
Snow tornadoes
- Snow devils.
- Solar heating on snow surface.
- Rare and weak.
- Northern Plains.
Landspouts
- Non-supercell tornadoes.
- From surface boundary rotation stretched by growing cumulus.
- Common in Colorado front range.
- Common in Florida sea breeze.
- Usually weak (EF0-EF1).
- Photogenic when dust-lit.
Gustnadoes
- Not true tornadoes.
- Non-tornado spin-up on gust front.
- No connection to cloud base.
- Sometimes damaging.
- Often mislabeled as tornadoes.
The very rare oddities
- Dust devils reaching cloud base (near-tornado but non-supercell).
- Vortex reversals in bow echoes.
- Meteotsunami-linked tornadoes on Great Lakes.
- Tropical cyclone spawned tornadoes.
- Snow squall spin-ups.
- Cold-air funnels (rarely reach ground).