Diphefo tsa Molelo, Diphefo tsa Pyrocumulonimbus, le Boitshwaro jo bo Feteletseng jwa Molelo wa Naga¶

Melelo e e tlwaelegileng ya naga e kgweediwa thata ke diphefo tse di mo godimo ga lefatshe, ditukisi tse di omileng, le go tshekama ga lefatshe, e tsamaya ka tsela e e ka bonelwang pele e batsamaisi ba maemo a tshoganyetso ba ka e dirang diura di le dintsi go sa le gale. Le fa go ntse jalo, fa molelo o o tseneletseng wa naga o golola maatla a a lekaneng a mogote go simolola go tlhagisa thulaganyo ya one ya maemo a bosa, molelo o fetogela go nna boitshwaro jo bo feteletseng jwa molelo wa naga jo bo laolwang ke diphuka. Mo metsotsong e se kae fela, maru a a kwa godimo a pyrocumulonimbus (pyroCb) a ka kgona go thunya dikilometara di le 10 go ya go di le 16 (maoto a le 33 000 go ya go a le 52 000) mo stratosphere, mme fa dikholomo tseo tse di tswang kwa godimo di tsidifala le go phutlhama, di itaya setsuatsue se se maatla go fitlha go k49m. (55 go ya go 85 mph)** go ya kwa tlase mo molelong, go thunya dikgabo le go fisa dikgabo go ya kwa ntle ka didikirii tsotlhe di le 360 ka nako e le nngwe.

Ka nako e le nngwe, diphefo tse di maatla tse di phaphametseng tse di dirisanang le go kgaoga ga lefatshe le go kopanya difatlhego tsa molelo di ka dikolosa didikologo tsa molelo tse di maatla le diphefo tse di maatla tsa setsuatsue** tse di nang le dithemphoritšhara tsa konokono tsa ka fa gare tse di fetang **1,090 degrees Celsius le 2,000). 200 km/h (125 mph). Di- vortice tseno di kumola ditlhare tse di godileng, di pitikolola dikoloi, di gagola marulelo mo dikagong, le go latlhela matlakala a a tukang go fitlha go 5 kilometers (3 miles) kwa pele ga mola o mogolo wa molelo. Go itse go bona matshwao a a tlhagisang a a bonwang a go phutlhama ga plume e e tlang kgotsa sediko sa molelo, goreng o tshwanetse go tswa pele ga molelo wa naga o fetoga go tswa mo go o o kgweediwang ke phefo go ya kwa go o o laolwang ke plume, le gore o ka falola jang mogote o o phatsimang mo teng ga koloi kgotsa Lefelo la Botshabelo la Nakwana fa o ka feta o boloka matshelo.

Dira se jaanong¶

1. Fuduga ka bonako fa kholomo ya mosi wa molelo wa naga e tlhatloga ka tsepamo jaaka setlhako sa setsuatsue kgotsa e fetoga go nna phepole-ntsho e e fifetseng. O se ka wa leta go kokota ga semmuso ga go fuduga ga ntlo le ntlo fa o bona leru le legolo le le tshweu le magala la kholifolawa (pyrocumbulus) molelo wa naga o o gaufi. Fa kholomo eo e e emeng e ka phutlhama, molelo o tla atologela kwa ntle mo ntlheng nngwe le nngwe ya khampase ka lobelo lo lo fetang lo pharakano ya bonno e ka kgonang go phepafatsa lefelo lengwe; bona melelo ya naga.
2. O se ka wa leka go feta sediko sa molelo kgotsa go tswa ga diphuka ka dinao kgotsa go tlhatloga thaba e e tlhomameng. Didiko tsa molelo di tsamaya ka tsela e e sa siamang go kgabaganya mela ya phefo ka lobelo lwa 30 go ya go 60 km/h (20 go ya go 37 mph), mme dikgabo di taboga go ya kwa godimo ga mothulama o o bogale jwa didikirii di le 30 kgotsa mo mogobeng o o tshesane fatshe. Tsamaya ka fa thoko go tswa mo dibotlolong tsa canyon le go tswa mo disaleleng tsa topological ka bonako.
3. Fa o tshwaregile mo tseleng ke setsuatsue sa ember kgotsa go thunya ga molelo, nna mo teng ga koloi ya gago e e ruletsweng ka tshipi. Koloi e e tswetsweng e naya tshireletso e e botoka thata kgatlhanong le mogote o o phatsimang wa didikirii tsa Celsius di le 1 000 (1 830-degree-Fahrenheit) go na le dipuse tsa mogote o o botlhole o o phatsimang mo dijong. Phaka mo lesweng le le senang sepe, letlapa, kgotsa sekontiri se se bulegileng kgakala le borashe jwa sekgwa le magora a logong ka moo go ka kgonegang ka teng.
4. Baakanyetsa koloi ya gago e e tshwaregileng gore e tle e tuke gone fela foo. Phutholola difensetere tsotlhe kwa godimo gotlhelele, tobetsa dipone tsa gago tsa kwa pele le dipone tsa kotsi tse di nang le ditsela tse nne gore bafalotsi ba kgone go go bona ka mosi o montsho, tlogela enjene e sa dire sepe fela fa mowa o o hemang o sa ntse o le teng (e time fa mosi o tlatsa tlelaemete go d**circute). go ya kwa tlase mo botong ya fa fatshe e e kwa tlase ga selekanyo sa difensetere tsa galase tse di khurumeditsweng ka kobo ya boboa kgotsa jase e e bokete ya letseta.
5. Fa o ka tshwarwa mo teng ga kago fa molelo o o tukang kgotsa sediko sa molelo o itaya, iphitlhele mo teng ga phaposi e e ka fa teng kgakala le difensetere tsa kwa ntle mme o lebelele phaposi e e kwa godimo. Le ka motlha o se tshabele mo mmileng fa molelo o mogolo o o tukang o feta kwa ntle; mogote o o phatsimang o tla fisa mafatlha a gago le go tshuba diaparo mo metsotswaneng. Tswala dikgoro tsotlhe tsa ka fa teng, gogela digaretene tse di bokete kgotsa difofu go thibela mogote o o phatsimang ka galase, mme o nne mo teng go fitlha kgabo ya metsotso e le 5 go ya go e le 15 e feta, morago ga moo o tswe ka bonako mo mmung o montsho o o setseng o fisitswe fa ntlo e ka tshwara molelo.
6. Leletsa nomoro ya gago ya tshoganyetso ya selegae ka bonako fa o tshwaregile kgotsa o iphitlhile mo lefelong. Leletsa 911 kwa United States le Canada, 112 go ralala Kopano ya Yuropa, 000 kwa Australia, kgotsa 999 kwa United Kingdom (bona dinomoro tsa tshoganyetso) mme o bege ditekanyetso tsa gago tsa GPS kgotsa aterese ya mmila, palo ya batho ba o nang le bone, le gore a o sireletsegile mo ntlong, mo lefelong le le phepa kgotsa mo koloing.

Go tlhaloganya ditiragalo tse di feteletseng tsa molelo wa naga: didikologo tsa molelo, di-firenado, le go phutlhama ga pyroCb¶

Borasaense ba molelo wa naga le baitseanape ba bosa ba bosetšhaba ba farologanya magareng ga melelo e e tlwaelegileng ya boalogodimo e e kgweediwang ke phefo le dipuso tse tharo tse di feteletseng tsa molelo wa lefaufau tse di sa dumalaneng le dinako tse di tlwaelegileng tsa go tima molelo le go fuduga.

flowchart TD
    A["Molelo wa Naga o o Matlhagatlhaga o o Gaufi"] --> B{"Ela tlhoko Boitshwaro jwa Mosi le Phefo"}
    B -->|"Mosi o obega ka go rapama kwa bogodimong jo bo kwa tlase ka phefo e e sa fetogeng"| C["Molelo o o Kgweediwang ke Phefo: Tsela e e bonelwang pele ya go anama; baakanyetsa Go-Bag le go tswa mo tseleng e e kgabaganyang phefo"]
    B -->|"Bogodimo jo bo kwa godimo jwa kholifolawa e tshweu e e emeng fa godimo ga kholomo e ntsho, legadima le le omileng, kgotsa go ritibala ga tshoganyetso"| D["TLHOKOMEDISO E E TLHOKANG KE DIPHULA / PYROCB"]
    D --> E{"A bogodimo jwa leru jo bo emeng bo simolotse go nna sephaphathi kgotsa pula ya virga/molora e nele?"}
    E -->|"Nnyaa: E sa ntse e tlhatloga"| F["Tswa JAANONG: Go phutlhama ga plume go ka diragala mo metsotsong e le 15 go ya go e le 30"]
    E -->|"Ee: Go rora ka tshoganyetso ga 100 km/h (60 mph) go thunya go go mogote ga lerole"| G["GO PULAMA GA PLUME GO A DIRA: Molelo o anama ka didikirii di le 360 + go bonala ga molelo wa bontsi dikilometara di le 3 go ya go di le 5 kwa pele"]
    G --> H{"A o kgona go kgweetsa o tswa mo tseleng e kgolo e e bulegileng e e phepa?"}
    H -->|"Ee"| I["Kgweetsa o tshubile dipone, difensetere di le kwa godimo, A/C e tshubilwe Recirculate"]
    H -->|"Nnyaa: Tsela e thibilwe ke dikgabo, megala e e weleng, kgotsa ga e bonale sentle"| J["Diragatsa Porothokholo ya go Falola go Fisiwa: Bokagare jo bontsi jwa kago KGOTSA koloi mo mmung o o senang sepe"]

1. Didikologo tsa molelo fa di bapisiwa le ditsuatsue tsa molelo tsa mmatota (ditsuatsue tsa ditsuatsue tsa pyrogenic)¶

Le fa gantsi batho ba bitsa kholomo epe fela e e dikologang ya kgabo "firenado," baitseanape ba fisikisi ya molelo ba kgaoganya di- vortice tsa molelo tse di dikologang ka dikarolo tse pedi tse di farologaneng go ikaegile ka tshimologo ya tsone, selekanyo sa tsone le maatla a tsone a go senya:

Mo teng ga sediko sa molelo, maatla a centrifugal a latlhela mowa o o bokete kwa ntle fa a ntse a goga digase tsa pyrolysis tse di sa fisiwang tse di fetofetogang (khabonemonokosaete, methane le ditara tsa logong tse di mouwane) go tsena mo gare ga kgatelelo e e kwa tlase ya vortex. Ka gonne okosejene e kgona go tlhakana fela go bapa le molelwane o o kwa ntle o o tlhakatlhakaneng wa konokono e e dikologang, vortex e otlogela kwa godimo go nna chimney e telele e e tseneletseng ya kgabo e e dikologang e e tukang makgetlo a le mararo go ya go a matlhano ka mogote le ka bonako go feta molelo o o bulegileng wa kampa wa bogolo jo bo tshwanang jwa lookwane.

2. Ditsuatsue tsa molelo tsa phaerokumulase (tse di bakang molelo) le tsa pirokhumulonimbase (pyroCb)¶

Fa molelo wa naga o tuka ka bogale mo dikhurumelong tse di kitlaneng tsa sekgwa, mo di- chaparral tse di omileng, kana mo dikago tsa toropo, o dira jaaka onto e kgolo ya madirelo, o pompa di- gigawatt tsa maatla a mogote le bongola (go tswa mo matuteng a a mowafalang le go tuka) ka tlhamalalo kwa lefaufaung:

1. Kgato ya pyrocumulus: Fa mosi o o goteditsweng thata o tlhatloga dimitara di le diketekete, mowa o a atologa le go tsidifala ka adiabatic go fitlha bongola bo tlhotlhorega go nna leru le le phatsimang, le lesweu le le phatsimang, le le rurugileng la cumulus le le ntseng jaaka kepisi ya kholifolawa ka tlhamalalo mo godimo ga columnke e e bosetlha jo bontsho.
2. The pyrocumulonimbus (pyroCb) stage: If the fire's heat output stays intense and upper-level atmospheric conditions are unstable, the updraft accelerates past 100 to 160 km/h (60 to 100 mph) vertically, punching right through the freezing level and reaching the tropopause or lower stratosphere at 10 to 16 kilometers (33,000 to 52,000 feet). Ice crystals and hail form inside the smoke-choked thunderhead, generating intense pyro-lightning (mostly dangerous positive-charge cloud-to-ground lightning bolts that strike dry forest up to 30 kilometers / 19 miles away from the main fire, igniting dozens of new wildfires behind evacuees).

3. The deadly physics of a pyroCb plume collapse (downburst)¶

The single most dangerous moment in any wildfire occurs when a towering pyrocumulonimbus column collapses:

• Why the column collapses: As the fire burns through a major fuel pocket or encounters high-altitude wind shear, or as falling rain and hail inside the upper cloud evaporate into dry mid-level air (cooling the air mass rapidly and making it dense and heavy), the upward thermal buoyancy suddenly fails.
• The 360-degree downburst impact: Millions of tons of cold, ash-laden air and smoke plunge straight down from 8 kilometers (26,000 feet) altitude at speeds exceeding 100 km/h (62 mph) and slam into the ground right on top of the active wildfire. Like water poured from a bucket onto a tabletop, this microburst downdraft hits the earth and blasts outward violently in all 360 degrees simultaneously.
• Consequences on the ground: Within 120 seconds, surface winds that were blowing steadily at 25 km/h (15 mph) from the west suddenly reverse or explode to 100 to 140 km/h (62 to 87 mph) in every direction. The downdraft flattens the tall flames horizontally against the ground, pre-heating unburned trees, and launches a horizontal blizzard of millions of glowing embers (firebrands) 3 to 8 kilometers (2 to 5 miles) ahead of the fire line, igniting entire neighborhoods before the main flame front even arrives.

Visual and sensory warning signs of an imminent blowup or plume collapse¶

You do not need radar equipment to recognize that a nearby wildfire is transitioning into an extreme, life-threatening blowup. Watch and listen for these six field indicators established by national wildland firefighting agencies:

1. The smoke column shifts from bent-over gray to a vertical white-capped tower: A moderate smoke plume bends horizontally with the prevailing wind. If the smoke column stands straight up like a massive pillar and builds a bright white, boiling, cauliflower cloud cap (or flattens out at the very top into an icy thunderstorm anvil), the fire is now generating its own weather.
2. Sudden eerie calm or inward-pulling breeze (indrafts): Right before a major blowup or fire whirl spin-up, the gigantic thermal updraft of the fire sucks surrounding air inward toward the base of the flames from kilometers away. If the wind around your home suddenly dies to a dead calm or reverses direction so that breeze is blowing into the approaching fire wall, a massive convective surge or plume collapse is imminent.
3. Darkening sky with falling ash, burnt pine needles, or blackened hail: If large, intact charred leaves, pine cones, or warm ash chunks start raining down on your property while you are still several kilometers from the visible flames, a powerful convective updraft is lofting debris miles high and dropping it onto your roof.
4. Streaks of dark virga (evaporating rain shafts) hanging underneath the smoke cloud: When dark, wispy curtains of rain fall out of the base of a pyroCb cloud and evaporate in the dry air before reaching the ground, that evaporative cooling accelerates a catastrophic downward microburst wind collapse.
5. A deafening freight-train roar: Both large fire whirls and crown-fire blowups produce an unmistakable, deep acoustic roar caused by millions of cubic meters of air being sucked into the combustion zone and spinning at tornadic velocities.
6. Barometric pressure drops and dry lightning flashes inside the smoke: Frequent jagged lightning bolts jumping out of the dark smoke column without wetting rain signal an active pyrocumulonimbus storm.

Terrain traps that multiply fire speed and trigger fire whirls¶

Topography dictates where fire whirls form and where flames accelerate beyond human survival thresholds. Never use these four terrain features as an evacuation path or refuge during an active wildfire:

How to evacuate before a plume-dominated fire traps your neighborhood¶

During extreme wildfire events, the majority of civilian fatalities occur during late evacuations on narrow, smoke-blinded roads clogged with stalled cars, fallen utility poles, and downed trees.

1. Leave at the "Ready / Set" (Advisory) stage, never wait for "Go" (Mandatory) if extreme fire weather is forecast: When national weather agencies issue a Red Flag Warning or Extreme Fire Danger alert (characterized by relative humidity below 15 percent, temperatures above 32°C / 90°F, and winds above 40 km/h / 25 mph), prepare your vehicle immediately. Back your car into the garage or driveway facing the street with the windows rolled up and your go-bag evacuation pack loaded inside.
2. Identify at least two orthogonal evacuation routes: Because a pyroCb plume collapse blasts fire outward in all directions and fire whirls jump highways, your primary road may be cut off in minutes. Map a primary route and a secondary route that travels at a 90-degree angle to the wind toward wide agricultural fields, large paved parking lots, beaches, or urban centers.
3. Dress every family member in 100 percent natural-fiber long clothing before walking out the door: Put on heavy 100 percent cotton denim jeans, a long-sleeved cotton or wool shirt, sturdy leather boots, leather work gloves, a cotton bandana or N95/P100 respirator, and wrap-around goggles (see wildfire smoke and ash inhalation). Never wear polyester, nylon, fleece, or spandex athletic wear during a wildfire evacuation: synthetic fabrics melt into burning liquid plastic against your skin when exposed to radiant heat or flying embers long before cotton ignites.
4. Disconnect your automatic garage door opener before the power grid fails: High winds and fire whirls snap power lines early in a wildfire. Pull the red manual emergency release cord on your overhead garage door track now so you are never trapped inside a dark garage with your car when the electricity cuts out.

Last-resort burnover survival: what to do if you are trapped and overrun¶

If your evacuation route is completely blocked by a wall of flame, fallen power lines, or zero-visibility black smoke during a plume collapse, you must immediately transition from driving to burnover survival. The critical fact to remember is that the deadly flaming front of a wildfire typically takes only 5 to 15 minutes to pass over a fixed point. If you can shield your body and airway from radiant heat and superheated gases during those 10 minutes of peak flame passage, you can survive and step out onto the cooled, already-burned black ground afterward.

Hierarchy of last-resort wildfire refuges (from safest to most dangerous)¶

Option 1: Inside a substantial, well-prepared building (Safest refuge)¶

Wildland survival data from Australia, the United States, and Southern Europe consistently proves that sheltering inside a solid building offers a vastly higher survival rate than fleeing on foot or driving blindly into dense smoke at the last minute:

• Bring everyone inside and close every exterior door, window, and vent: Shutting windows blocks 70 to 90 percent of exterior radiant heat and stops the indoor wind tunnel of flying embers.
• Turn OFF the main household natural gas valve and outdoor propane tank valve: If your house catches fire after the front passes, closed gas valves prevent secondary gas explosions.
• Leave interior lights ON and fill sinks, bathtubs, and buckets with water: When thick black pyroCb smoke turns midday into pitch-black midnight and the power grid fails, water reserves help extinguish small ember spots around window sills.
• Close curtains or metal blinds, move upholstered furniture away from windows, and shelter in a room on the side farthest from the approaching fire that has a direct exterior door to clear/burned ground.
• Watch the ceiling and attic manhole continuously: Houses rarely ignite from a wall of flame hitting the outside siding; instead, tiny wind-blown embers suck through roof eaves and attic vents during an ember storm, igniting the attic from the inside. Keep a ladder under the attic hatch and check it every few minutes.
• When to exit the house: Stay inside while the roaring flame front passes outside (usually 5 to 15 minutes). If the roof or walls of your house catch fire and fill the rooms with black toxic smoke, wait until the exterior hurricane of flame has subsided, cover your body completely in dry wool blankets (never soaking wet blankets, which conduct steam heat into your skin under intense radiant flux), hold a damp cloth over your nose and mouth, and walk out the leeward door directly onto already-burned black ground ("the black") or a wide paved driveway.

Option 2: Inside a stationary closed vehicle on bare ground (Second-best refuge)¶

If you are caught on a highway or rural road and cannot reach a solid building:

1. Do NOT abandon your car to run down the road on foot: People who panic and jump out of stalled cars to run through a wildfire are almost always overcome by radiant heat (which reaches 20 to 40 kilowatts per square meter), zero visibility, and 300-degree-Celsius (570-degree-Fahrenheit) air within 50 meters (165 feet).
2. Park on the widest, barest patch of ground available: Pull onto a gravel turnout, dirt intersection, wide asphalt shoulder, or rock cut, or park behind a solid concrete bridge abutment or earthen bank that blocks the direct line of sight to the tallest trees. Avoid parking directly over dry tall grass or right against heavy roadside brush.
3. Angle the rear or side of the vehicle toward the approaching fire if time permits, turn on hazard flashers and headlights, and shut all windows and sunroofs tightly.
4. Set air conditioning vents to Recirculate (closed outside air damper), then shut off the engine once smoke thickens.
5. Get down on the floorboard below the window glass line: Tempered side windows can shatter if hit by flying fire-whirl debris or extreme uneven thermal stress. Crouch or lie flat on the floor wells beneath the level of the steel doors (which block 100 percent of infrared radiant heat) and pull a wool blanket, heavy cotton jacket, or even the car's cloth floor mats completely over your head, neck, and hands.
6. Expect terrifying noise, heat, and rocking: As the flame front passes over the car for 3 to 8 minutes, howling outflow winds will rock the suspension, smoke may seep around door gaskets, the tires may pop or catch fire, and exterior plastic trim may melt. Stay down under your wool blanket until the peak roar and orange glare subside. Modern fuel tanks rarely explode during the initial pass; only exit the vehicle onto the burned black ground once the external flame wall has moved past or if active fire penetrates the passenger cabin itself.

Option 3: Open-ground Temporary Refuge Area (Last resort if caught on foot outdoors)¶

If you are hiking or working outdoors without a vehicle or building when a fire whirl or blowup traps you:

• Head immediately for "the black" (already burned ground) if accessible: Ground that has already burned clean of fuel cannot burn a second time; it is the safest place in the area once cooled slightly.
• If you cannot reach the black, find the largest bare clearing, rock scree field, dirt road, gravel riverbed, or plowed field available.
• Alternatively, submerge in a deep pond, lake, river, or cold swimming pool: Beware of shallow plastic above-ground pools (which melt and collapse) or shallow creeks surrounded by overhanging forest canopy (where superheated air and carbon monoxide still blanket the water surface). Keep your clothing on and breathe right at the cool water surface through a wet cotton cloth.
• If forced to survive on bare dirt with no water: Scrape away all dry leaves and twigs down to bare mineral soil in a circle as wide as possible. Dig a shallow trench in the dirt, lie flat face-down with your feet pointed toward the approaching flames, press your face into a hollow in the cool soil breathing through a moistened cotton cloth (never breathe upward into the superheated air layer), and cover every millimeter of exposed skin with dirt, wool, or cotton layers until the flame front passes over you.

Dipotso tse di bodiwang kgapetsakgapetsa¶

What is the difference between a fire whirl and a true fire tornado (firenado)?¶

A common fire whirl is a localized spinning column of flame and ash, usually 1 to 50 meters (3 to 165 feet) wide, formed near the ground when intense surface heat rises and stretches horizontal wind shear around ridges or merging fire lines. A true fire tornado (pyrogenic tornadic vortex) is a massive, meteorology-driven tornado directly connected to the rotating updraft of a towering pyrocumulonimbus thunderstorm cloud high above the fire; it can exceed 300 meters (1,000 feet) in width, generate EF-2 to EF-3 winds above 220 km/h (135 mph), burn at over 1,090 degrees Celsius (2,000 degrees Fahrenheit), and stay on the ground for over an hour.

Why is a pyrocumulonimbus (pyroCb) plume collapse so dangerous to people evacuating a wildfire?¶

While a pyrocumulonimbus smoke column is actively rising 10 to 15 kilometers (33,000 to 50,000 feet) into the sky, its powerful updraft sucks air inward toward the fire. When the upper cloud cools or hits wind shear and the updraft suddenly fails, millions of tons of dense air plunge straight down onto the fire in a violent microburst. Upon hitting the ground, this downdraft blasts outward in all 360 degrees at 90 to 140 km/h (55 to 85 mph), causing the wildfire to explode rapidly in every direction at once while showering burning embers up to 5 kilometers (3 miles) ahead of the main fire line.

If my car is trapped on a road by an advancing wildfire, should I get out and run on foot?¶

No, never abandon a closed metal vehicle to flee on foot during a wildfire burnover. Walking or running in the open exposes your bare skin and lungs directly to lethal radiant heat fluxes and superheated gases above 200 degrees Celsius (400 degrees Fahrenheit), which cause fatal airway burns and collapse within seconds. Instead, park your vehicle on the barest patch of pavement, gravel, or dirt away from heavy trees, roll up all windows, set air vents to Recirculate, turn on hazard lights, and crouch down on the floorboard below the window glass covered completely in a wool blanket or cotton clothing until the 5-to-15-minute flame front passes.

Why should I cover myself with a dry wool blanket instead of a soaking wet blanket during a wildfire burnover?¶

During the intense radiant and convective heat pulse of a wildfire burnover, water soaked into a blanket or clothing resting against your body can rapidly heat to 100 degrees Celsius (212 degrees Fahrenheit) and turn into scalding steam, conducting heat seven times faster into your skin than dry air and causing severe steam burns. Use a dry 100 percent wool blanket or heavy cotton coat as your outer thermal shield to block radiant heat, and use only a lightly dampened cotton cloth held over your nose and mouth to cool and filter the air you breathe.

Metswedi e tlhotlhomisitswe¶

• National Wildfire Coordinating Group (NWCG) and United States Forest Service (USFS, United States): S-290 Intermediate Wildland Fire Behavior: Plume-Dominated Fires, Fire Whirls, and Entrapment Avoidance
• Country Fire Authority (CFA, Victoria) and NSW Rural Fire Service (Australia): Bushfire Survival Guide: Radiant Heat Protection, Sheltering in a Building, and Vehicle Burnover Procedures
• National Weather Service (NWS) and NOAA (United States): Pyrocumulus, Pyrocumulonimbus (PyroCb) Downdrafts, and Fire Tornado Case Studies
• Federal Emergency Management Agency (FEMA / Ready.gov, United States) and CAL FIRE: Wildfire Evacuation: Ready, Set, Go and Ember Storm Preparedness
• Canadian Interagency Forest Fire Centre (CIFFC) and Natural Resources Canada: Extreme Wildfire Behavior and Pyrogenic Vortex Dynamics

Dikaedi tse di tsamaelanang¶

• Wildfires: evacuation, defensible space, and survival
• Mosi wa molelo wa naga le go hema molora
• Post-wildfire burn scar mudslides and debris flow evacuation
• Burns and scalds first aid
• Go-bag evacuation pack