Vadtüzek utáni égési hegek sárlavina és törmelékek kiürítése¶

Amikor egy súlyos erdőtűz kialszik, az elszenesedett hegyek alatt élők vészhelyzete csak a második szakaszába lépett. For two to five years after a high-severity wildfire strips away forest canopy, ground litter, and root networks, the burned watershed becomes a primed geological hair-trigger. Worse still, intense wildfire heat vaporizes waxy organic compounds in the forest floor and drives them several centimeters down into the soil, where they condense into a water-repellent (hydrophobic) crust that sheds rainwater almost like an asphalt parking lot.

Unlike normal wet-season landslides that require days of soaking rain to saturate deep hillside clay, a post-wildfire debris flow is triggered within 5 to 15 minutes by a single brief burst of high-intensity rainfall. Just 7 to 12 millimeters (0.3 to 0.5 inches) of rain falling in 15 minutes on a steep burn scar can generate a sheet of surface runoff that scours million-ton channels of ash, mud, stripped tree trunks, and house-sized granite boulders into a fast-moving slurry with the density of wet concrete. Travelling down canyons and spreading unpredictably across neighborhood alluvial fans at 30 to 65 km/h (20 to 40 mph), post-fire debris flows crush homes off their foundations in seconds. Knowing why you must evacuate hours before a rain cell hits a burn scar, why sandbags cannot stop a boulder slurry, and how to survive vertically if trapped overnight saves lives.

Tedd ezt most¶

1. Evacuate immediately when a Flash Flood Watch or Debris Flow Evacuation Order is issued for your burn-scar zone, hours before the rain starts. Never wait until heavy rain is drumming on your roof to drive out. Post-wildfire debris flows mobilize within 5 to 10 minutes of a convective downpour hitting the upper mountain ridge, which means boulders and mud can surge down your street even before heavy rain reaches your house at the base of the hill; lásd földcsuszamlások.
2. Never attempt to drive across a flowing canyon road, brown mud stream, or low-water dip below a burn scar. Post-fire slurries are twice as dense as water and carry submerged 5-ton boulders and jagged logs that sweep heavy sport utility vehicles and fire trucks off bridges in an instant.
3. Listen for a low, rumbling freight-train roar, cracking trees, or the clanking impact of boulders knocking together uphill. If you hear deep ground vibration or see a dry creek bed suddenly either drop to a trickle (indicating a logjam dam upstream) or turn into thick, black, ash-choked sludge, a debris flow front is seconds away.
4. Run uphill and sideways (perpendicular to the canyon channel) if caught outdoors on foot. Never run straight downhill ahead of a debris flow; egy szikla iszap 10-18 méter/s (33-60 láb/s) sebességgel mozog, és minden sprintert megelőz. Azonnal másszon fel a legközelebbi meredek völgyfalon vagy gerincszárnyon, távol a vízelvezető középvonalától.
5. Climb to the highest floor, attic roof space, or exterior rooftop on the downhill side of the house if trapped indoors at night. If a mudslide hits before you can evacuate, never stay in a basement, ground-floor bedroom, or hillside-facing room. Bring an axe, crowbar, or heavy tool to break through the roof sheathing from inside if the mud rises, and position yourself on the roof crest or second-story room on the leeward (downhill) side of the building.
6. Stay away from canyon channels after the first wave passes and call emergency services if trapped. Post-wildfire debris flows always travel in multiple distinct surges (pulses) separated by 5 to 45 minutes as upstream logjams burst; a második vagy harmadik sziklatömb gyakran nagyobb, mint az első. Hívja a helyi segélyhívó számot (911 az Egyesült Államokban és Kanadában, 112 az Európai Unió egész területén, 999 az Egyesült Királyságban), vagy ellenőrizze segélyhívó számok.

Miért hoznak létre a leégett vízgyűjtők halálos iszapcsuszamlásokat a rövid esők miatt?¶

After a wildfire, many homeowners look at a weather forecast calling for only 15 millimeters (0.6 inches) of total rain and assume there is no danger because their canyon easily handled 100-millimeter (4-inch) winter storms before the fire. Geological engineers at the United States Geological Survey (USGS) and international hazard agencies emphasize that wildfire fundamentally rewires watershed hydrology through four mechanisms:

flowchart TD
    A["High-Severity Wildfire Strips Watershed"] --> B["Hidrofób (víztaszító) talajréteg + lombkorona és alom elvesztése"]
    B --> C{"A konvektív esősejt égési hegeket talál: >6 mm (0,25 hüvelyk) 15 perc alatt?"}
    C -->|"Nem: Enyhe enyhe szitálás"| D["Hamu és iszap lefolyása; monitor NWS Flash Flood Watches closely"]
    C -->|"Yes: Short intense downpour"| E["Sikertelen beszivárgás: A lepedő lefolyása megmossa a dombokat és a kanyonágyat"]
    E --> F["5-15 PERC ALATT MOBILIZÁLIK A TÖMÉKÁRAMLÁST: sziklák + rönkök + hamu iszap"]
    F --> G{"Már evakuálták az alluviális rajongói zónán kívül?"}
    G -->|"Igen"| H["Stay out until official All-Clear; beware of multi-surge pulses"]
    G -->|"No: Trapped in home or canyon when roar begins"| I["AZONNAL menjen a 2. emeletre vagy a tetőre a lejtős oldalon (vagy mássz fel az oldalsó lejtőn gyalog)"]

1. Hydrophobic (water-repellent) soil formation¶

Az élő fenyőtűk, levélkék levelei, eukaliptusz alom és talajgombák természetes hidrofób (vízgyűlölő) szerves viaszokat és lipideket tartalmaznak. Intenzív erdőtűz idején, amikor a talaj felszínének hőmérséklete eléri a 200-600 Celsius-fokot (400-1100 Fahrenheit-fok):

1. A talaj tetején lévő alomréteg teljesen finom porszerű hamuvá ég, míg az alatta lévő szerves viaszok gázzá párolognak el.
2. Part of that waxy vapor moves downward along the steep temperature gradient into the cooler mineral soil 2 to 8 centimeters (1 to 3 inches) below the surface.
3. Upon touching the cooler soil grains, the vapor condenses and coats every grain of sand and dirt in a continuous, chemically bonded film of water-repellent wax.
4. A viaszos gát fölött egy vékony, 2-5 centiméteres (1-2 hüvelyk) takaró található, amely finom, bolyhos hamuból és szénből áll. When a rainstorm hits, that thin top ash layer saturates in less than 3 minutes, cannot soak downward through the hydrophobic wax barrier underneath, and slides off the entire mountainside at once like wet frosting sliding off a greased tilted pan.

2. Hyper-dried soil micropore sealing and ash clogging¶

Even where hydrophobic waxes are patchy, fine microscopic wildfire ash washes into the natural soil pores and earthworm channels with the first raindrops, plugging them like wet cement. Simultaneously, raindrops falling directly from the sky at 9 meters per second (30 feet per second), no longer intercepted or slowed down by tree branches, pine needles, or brush canopy, hammer the bare dirt directly (raindrop splash erosion), detaching millions of tons of loose sediment.

3. Progressive bulking vs. infiltration-triggered landslides¶

This distinction is the single most important concept in post-fire survival:

4. How the boulder snout forms and destroys structures¶

As the fast-moving slurry of ash and water rushes down a steep V-shaped mountain canyon, it picks up everything sitting in the dry creek bed from the past century: fallen burned trees, loose gravel, and massive boulders (progressive bulking, which multiplies the flow volume by tenfold or more). Because of grain-inertia physics inside a churning slurry (kinetic sieving), the largest multi-ton boulders and tangled tree trunks are pushed straight to the very front and top edge of the moving wave, forming a towering, semi-solid boulder snout 2 to 6 meters (6 to 20 feet) high.

Behind this boulder wall, the watery mud pushes like a hydraulic piston. When the boulder snout exits the mouth of the mountain canyon onto the flatter neighborhood below, the boulders act as a battering ram that punches straight through residential walls, snaps utility poles, and shears bridges off their piers, while the liquid mud behind it immediately fills rooms to the ceiling and buries occupants.

Understanding alluvial fan hazards: why living far from the creek bed is not safe¶

Many residents living 200 to 500 meters (650 to 1,650 feet) away from a canyon creek channel believe they are out of danger because normal winter creek floods stay inside the concrete flood channel or narrow creek bed. In a post-wildfire debris flow, that assumption is deadly because of alluvial fan avulsion.

What is an alluvial fan and how does channel plugging (avulsion) work?¶

Szinte minden hegylábi negyed egy hegyvonulat tövében épült egy szelíd, kúp alakú, ősi üledékből álló kötényen, amelyet hordalékkúpnak neveznek. Ezt a ventilátort több ezer éven keresztül építették a kanyon torkolatából kilépő, szikláit ledobó, tűz utáni törmelékek.

Amikor egy modern, vadtüzek utáni törmelékáramlat kilép a meredek kanyonból egy hegylábi negyed enyhébb lejtőjére:

1. Bridge and culvert plugging in 30 seconds: The first wave of tangled 10-meter (33-foot) burned tree trunks and 3-meter (10-foot) boulders reaches the first neighborhood road bridge or storm-drain culvert. Because the culvert was engineered only for clear rainwater, the boulders and logs instantly jam across the opening, plugging the creek channel 100 percent shut.
2. Azonnali csatornaugrás (avulsion): Másodperceken belül a következő több millió liter sár és sziklák felülkerekednek az eltömődött hídon, és teljesen kiugranak a patak medréből (avulsion), és a lakóutcákat, felhajtókat és zsákutcákat fél kilométerrel odébb az új fő sziklacsatornává alakítja.
3. Unpredictable lobe splitting: As boulder lobes stall on flat ground, they form instant dams that deflect the next surge 45 to 90 degrees left or right through homes that had never flooded in recorded history.

A hivatalos csapadékküszöbök és a tűzeset utáni veszélytérképek olvasása¶

Before the first rainy season arrives after a wildfire, national geological and weather agencies (such as the USGS Post-Fire Debris-Flow Hazard Assessment team and the National Weather Service in the United States, or equivalent national civil protection authorities) publish emergency watershed assessments for every major burn scar.

Rainfall intensity thresholds (I15 és I60)¶

Post-fire debris flows are governed by short-duration rainfall intensity (how hard it rains in 15 minutes), not total 24-hour storm accumulation:

• The 15-minute rainfall intensity threshold (I15): On a fresh Year-1 high-severity burn scar with steep slopes (>23 to 30 degrees), a 15-minute rainfall rate equivalent to 16 to 24 millimeters per hour (0.6 to 0.95 inches per hour), which means just 4 to 6 millimeters (0.15 to 0.25 inches) of rain falling in a 15-minute window, is often enough to initiate dangerous mud and debris flows.
• Why embedded thunderstorm bands and atmospheric rivers are the top killers: A broad winter storm may drop gentle rain at 3 millimeters (0.12 inches) per hour all day without triggering a slide. However, if a narrow narrow cold-frontal rainband (NCFR) or embedded convective thunderstorm cell passes over the mountain peak at 3:00 AM and dumps 10 millimeters (0.4 inches) of rain in 12 minutes, the entire watershed can fail simultaneously in the dark while residents are asleep.

A 2-5 éves vízválasztó helyreállítási idővonal¶

Mennyi ideig marad veszélyes az égési heg a tűz eloltása után?

Vihar előtti evakuálási és felkészülési ellenőrző lista égési sebhelyes lakosok számára¶

Ha otthona egy leégett vízgyűjtő belsejében vagy lejtőjén található (a hegy alapjától 1-5 kilométeren belül, egy kanyon vízelvezető vagy hordalékkúp mentén), tegye meg az alábbi lépéseket az esős évszak kezdete előtt:

• Ellenőrizze ingatlana hivatalos tűz utáni törmelékáramlási veszélytérképét: Lépjen kapcsolatba a megyei katasztrófavédelmi hivatallal, az önkormányzati polgári védelmi ügynökséggel vagy a geológiai felmérés webhelyével, hogy megbizonyosodjon arról, hogy az Ön utcája aktív törmelék-áramlási zónában vagy kanyon ventilátorcsatornájában fekszik.
• Regisztráljon a Wireless Emergency Alerts (WEA) és a fordított 911-es vezetékes/mobil hívásokra: Tartsa mobiltelefonját úgy, hogy elkerülje a „Ne zavarjanak” vagy „Alvófókusz” funkciót a vészhelyzeti riasztások és az Országos Meteorológiai Szolgálat esetén.
• Vásároljon akkumulátoros NOAA időjárási rádiót (vagy nemzeti vészhelyzeti rádiót) hangos riasztással: A leégett hegygerinceken lévő mobiltornyok gyakran elveszítik a tartalék tápellátást, vagy az első sárlavina miatt megszakadnak az optikai vezetékeik.
• Ne feledje, hogy a homokzsákok és a k-sínek csak a sekély sarat térítik el: Ha homokzsákokat vagy faterelő falakat helyez el az ingatlanon, döntse meg őket egy sekély 30-45 fokos átlóban, hogy a sekély lapos iszapot körül vezesse a ház sarkain az utca felé, ahelyett, hogy egy sima, 90 méteres, dadméteres átjárót építsen. felrobban. Soha ne hagyatkozzon homokzsákokra az evakuálás helyett a vörös/kötelező törmelékáramlási figyelmeztetés idején.
• Állítson fel függőleges túlélőeszközöket a felső emeleten vagy a padláson: Ha egy éjféli felhőszakadás figyelmeztetés nélküli törmelékáramlást vált ki, mielőtt elindulna, tartson egy tűzoltó fejszét vagy nehéz feszítőrudat, akkumulátoros dugattyús fűrészt, nagy fényerejű fényszórókat, sípot, meleg gyapjútakarókat és egy állandó elsősegélynyújtó készletet a második padlón tárolva vagy rögzítve. vágjon ki egy menekülési lyukat a tetőn, ha sár tölti be az első emeletet.

Mi a teendő, ha a törmelék áramlása során beszorult egy lakásba vagy járműbe¶

Ha közeledő törmelék zúgását hallja, vagy a sár nekiütközik otthonának falának, kevesebb, mint 30 másodperce van a cselekvésre:

Házon belül: függőleges és lejtős elhelyezés¶

1. Menjen fel azonnal: Sprint a második vagy harmadik emeletre, vagy mássz fel a padlásra vagy a tető legmagasabb részére. Egy emeletes, második emelet nélküli otthonban mássz fel erős konyhai munkalapokra, magas, nehéz szekrényekre, vagy egyenesen fel a tetőtér bejárati nyílásán keresztül a tetőtartóba.
2. Stay on the DOWNHILL (leeward) side of the structure: Never shelter in a room facing the uphill slope or canyon channel. The uphill walls absorb the direct, crushing impact of boulders and tree trunks; moving to the far downhill rooms puts the entire structural frame of the house between you and the boulder snout.
3. Never enter a basement or subterranean garage: Basements fill with liquid cement-like mud in 10 seconds, trapping occupants with zero air pocket and crushing doors shut under tons of hydrostatic mud pressure.
4. Watch for gas leaks and downed live wires: Debris flows routinely shear natural gas meters off exterior house walls and pull down high-voltage transformers. Do not light matches or candles; use LED flashlights.

After a debris flow hits: rescuing others and avoiding secondary surges¶

• Do NOT walk out onto fresh, deep debris-flow mud: Freshly deposited post-fire mud behaves like thixotropic quicksand: a thin dried crust may form on top within an hour, while the mud 30 centimeters (12 inches) underneath remains liquid slurry up to 3 meters (10 feet) deep. Stepping onto fresh mud causes rescuers to sink past their chest and become immobilized while the next boulder surge races down the canyon.
• Várja meg, amíg a több hullámos ciklus véget ér: Továbbra is nézze és hallgassa a magaslatról. Elsősegélynyújtásban csak olyan hozzáférhető áldozatokat adjon, akik szilárd tetőkről, érintetlen, magas talajról vagy a szélen átfektetett, biztonságos deszkákon/létrákon keresztül érhetők el.
• Treat survivors for crush injuries, hypothermia, and corneal/airway ash burns: Victims pulled from cold winter mud slurries rapidly develop life-threatening hipotermia, crush syndrome, valamint a sáros futótűzhamuvíz belélegzéséből származó aspirációs tüdőgyulladás. Öblítse le tiszta vízzel a sarat a szeméből és a szájából, csavarja be a személyt száraz hőtakaróba, és várja meg a helikopteremelőt vagy a műszaki városi kutató-mentő csapatokat.

Vehicle entrapment, dry-ravel rockfalls, and municipal debris basins¶

Beyond residential neighborhoods on alluvial fans, post-wildfire watersheds pose severe, ongoing hazards to commuters driving mountain highways, hikers walking canyon trails, and properties located adjacent to municipal flood-control infrastructure.

1. Dry-ravel rockfalls before the first raindrop falls¶

You do not need a rainstorm for a fresh burn scar to bury a mountain highway. Throughout the dry summer and autumn immediately following a wildfire, a geological process called dry ravel occurs continuously on slopes steeper than 30 degrees:

• How dry ravel works: For decades before the fire, small rocks, gravel, and sand particles rolling downhill were caught and held in place by woody shrub stems, grass tufts, and living tree roots (forming mini-terraces called "vegetation dams" behind every bush). When a wildfire burns those stems and shallow roots to ash, millions of tons of perched gravel, cobbles, and football-sized rocks suddenly lose their mechanical support.
• Gravity-driven cascades: Driven purely by gravity, thermal expansion/contraction between day and night, and light afternoon breezes, dry rocks and ash cascade down the burned slope like sand in an hourglass, piling up metres deep inside the dry creek bottoms and spilling across mountain highway lanes.
• Driving safety in dry-ravel corridors: Never stop or park your vehicle underneath a steep, freshly blackened road cut to take photographs. Watch for fist-sized rocks bouncing onto the asphalt, which frequently precede a larger boulder release after the burned tree roots holding a cliffside slab give way.

2. What to do if your vehicle is caught on a canyon highway during a post-fire downpour¶

Mountain highways winding through burned canyons are the single deadliest place to be when a convective rain cell strikes the watershed:

1. Never enter a canyon road during a Flash Flood Watch for a burn scar: Highway departments often close burned canyon routes hours before a storm, because a single rain burst will simultaneously drop debris cones across the road at 20 different side-gullies, trapping every car inside the canyon between rockslides with the rising river below.
2. If caught driving when intense rain and mud cascades begin:
3. Do NOT shelter underneath a canyon bridge or inside a narrow culvert overpass: Bridges and culverts are the exact focal points where side-channel debris flows slam into the main road and plug up.
4. Do NOT try to drive through a rock-and-mud lobe spilling across the asphalt: Even a 30-centimeter-deep (12-inch) tongue of wet burn-scar mud crossing the highway has the high viscosity and rock content to high-center your vehicle's undercarriage immediately, pinning your car directly in the chute where a 4-meter (13-foot) boulder wave will come down 60 seconds later.
5. Park on the widest, highest engineered fill section away from side-gully chutes: Look at the mountainside above the road. Avoid stopping underneath V-shaped side gullies, ravines, or dry waterfall chutes. Pull onto the widest straight section of road hugging a broad ridge nose (a convex outward curve of the mountain rather than a concave inward gully).
6. Abandon the vehicle and climb UP the ridge nose on foot if mud is rising around the wheels: Unlike a clean-water street flood or a highway black-ice pileup, if your vehicle becomes immobilized in the path of an active post-fire boulder debris flow and mud is actively piling up against your doors, the car will be crushed or swept into the river canyon. Unbuckle every passenger immediately, exit out the side or window away from the flowing mud, and scramble straight up the solid convex ridge flank (never into a gully) at least 15 to 30 meters (50 to 100 feet) vertically above the roadbed.

3. How municipal debris basins and check dams work (and how they overtop)¶

In many wildfire-prone regions (such as Southern California, the European Alps, Japan, and Taiwan), flood-control engineers build gigantic earthen or concrete catch basins called debris basins at the mouths of mountain canyons right above residential suburbs:

Post-event health, utility, and environmental hazards in burn-scar mud¶

Once the debris flow stops moving and emergency authorities allow access, the thick black-and-gray mud blanketing streets and homes presents severe chemical, biological, and structural dangers:

• Toxic heavy metals and caustic wood ash: Post-wildfire mud is not clean forest dirt. It contains concentrated calcium hydroxide (caustic wood ash with a high alkaline pH that causes chemical skin and eye burns), polycyclic aromatic hydrocarbons (PAHs), dioxins, and heavy metals (lead, arsenic, hexavalent chromium, and cadmium) leached from burned homes, melted car batteries, solar panels, and copper plumbing uphill. Always wear waterproof rubber boots, heavy nitrile/neoprene gloves, safety goggles, and an N95/P100 respirator when cleaning up dried burn-scar mud; see vegyi anyagok kiömlése.
• Raw sewage contamination: Boulder surges routinely snap municipal sewer mains and rip residential septic tanks out of the ground, mixing raw human sewage and E. coli bacteria throughout the mud slurry. Immediately wash any skin cut or scrape exposed to debris-flow mud with soap and bottled/boiled water, and verify that your tetanus vaccination is current.
• Compromised drinking water systems: Debris flows shear underground water distribution pipes and overwhelm municipal water treatment plants with high-turbidity ash runoff. Assume tap water is unsafe to drink until your local water utility lifts all advisories; see water safety and boil notices.
• Hidden structural foundation undermining: Even if a house appears upright after mud flows around it, boulders striking the uphill foundation stem wall or fast-moving slurry scouring 2 meters (6.5 feet) of soil out from underneath a corner footing can leave the building ready to collapse. Do not turn on electricity or enter a mud-impacted house until a municipal building engineer inspects the foundation and gas lines.

Consider completing a certified hands-on First Aid, CPR, and Disaster Preparedness course through the Red Cross, St John Ambulance, or your local Community Emergency Response Team (CERT).

Gyakran ismételt kérdések¶

Why can a tiny 15-minute rain shower trigger a massive mudslide after a wildfire when heavy storms never caused slides before?¶

Before a wildfire, tree canopies, pine needles, and porous organic soil act like a giant sponge that absorbs several inches of rain before runoff begins. A high-severity wildfire strips all protective vegetation and vaporizes organic soil waxes, which condense just below the surface into a water-repellent (hydrophobic) crust. When a brief downpour drops just 6 to 12 millimeters (0.25 to 0.5 inches) of rain in 15 minutes, the water cannot soak into the hydrophobic ground; instead, it sheets rapidly off the entire mountainside at once, scouring loose ash, soil, burned logs, and boulders out of steep canyons to form a fast-moving debris flow within 5 to 15 minutes.

How is a post-wildfire debris flow different from a normal flash flood?¶

A normal flash flood is mostly liquid water carrying small amounts of silt, whereas a post-wildfire debris flow is a dense, viscous slurry composed of up to 60 to 80 percent solid sediment, ash, uprooted trees, and multi-ton boulders with the consistency and weight of wet concrete (roughly twice as heavy as water). Because huge boulders are pushed to the leading front of the wave, a debris flow exerts ten to fifty times the impact force of floodwater, smashing straight through residential walls, snapping concrete bridges, and plugging storm channels so the flow jumps onto neighborhood streets.

Why is my house at risk from a post-fire debris flow even if I live several blocks away from the creek channel?¶

Foothill neighborhoods at the base of mountain ranges are typically built on alluvial fans, which are broad cones of sediment deposited by ancient debris flows. When a post-wildfire debris flow exits a steep canyon mouth carrying giant boulders and tangled tree trunks, it immediately plugs the first road bridge, culvert, or concrete flood channel it hits. Within seconds, the following waves of mud and boulders overflow the blocked channel (an avulsion) and turn residential streets, avenues, and yards hundreds of meters away from the creek into the new active boulder path.

What should I do if a post-wildfire mudslide hits my house in the middle of the night before I can evacuate?¶

Do not go outside on foot into the dark street, and never stay in a basement, first-floor bedroom, or any room on the uphill side of the house. Immediately wake everyone and climb to the highest level of the building, such as the second floor, attic, or rooftop, and position yourself on the downhill (leeward) side of the structure away from the impacting boulders. Bring an axe, pry bar, or heavy tool into the attic so you can break out onto the roof if mud fills the house, and stay on high ground because post-fire debris flows arrive in multiple waves separated by 5 to 45 minutes.

A források ellenőrizve¶

• United States Geological Survey (USGS, Landslide Hazards Program): Emergency Assessment of Post-Fire Debris-Flow Hazards, Rainfall Intensity Thresholds (I15), and Alluvial Fan Avulsion Mechanics
• National Weather Service (NWS) and NOAA (United States): Burn Scar Flash Flood and Debris Flow Warning Guidelines and Watch/Warning Preparedness
• California Geological Survey (CGS) and CAL FIRE (United States): Post-Wildfire Watershed Emergency Response Team (WERT) Reports and Homeowner Mudslide Survival Guides
• Federal Emergency Management Agency (FEMA / Ready.gov, United States): Landslides, Debris Flows, and Post-Fire Flood Risks
• Natural Resources Canada and Geoscience Australia: Post-Bushfire / Post-Wildfire Slope Instability and Hydrophobic Soil Runoff Guidance

Kapcsolódó útmutatók¶

• Landslides and mudslides: warning signs and survival
• Flash floods: immediate actions and survival
• Vadtüzek: evakuálás, védhető tér és túlélés
• Crush sérülés és kompartment szindróma
• Hipotermia és fagyás elsősegélynyújtása