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Bibale oyo ezali na mopɛpɛ, kobukana ya ba Levee, mpe Mpela ya Bassin oyo ezali na likama

Mituya ya mbalakaka ekeseni na mikili. Lokasa oyo esaleli 911, nimero ya États-Unis mpe Canada. Bikólo mosusu mingi esalelaka 112, 999, to motángo mosusu. Luka nimero ya mboka na yo.

(Gulf of Mexico)

Ba priorités na yo ya kobika ya mbala moko na tango ya crise ya ebale to ya levee ya atmosphérique ya makasi ezali ya ko évacuer avant levee ya mabele ebuka (lokola mayi oyo ezali kosopana na nzela ya levee epanzani etondisaka ba bassins ya ba plaines inondables oyo ezindi na 2 à 6 mètres / 6 à 20 pieds na profondeur na ba heures mpe etikalaka na ba semaines), yeba bilembo ya komona ya kokweya ya levee oyo ezali pene lokola "ba boils ya zelo" ya potopoto oyo ezali ko bubbler sima ya toe ya levee, kozonga sima ata moke te na grenier ya kokangama sans hache to fenêtre ya toit, mpe jamais kotambwisa motuka zingazinga ya ba barricades ya mpela to kokatisa banzela oyo ezipami na mayi.

Sala boye sikoyo

  1. Evacuate immediately if a Levee Breach Warning or Evacuation Order is issued for your zone: Do not wait to see water in your street if you live in a levee-protected basin, polder, or valley floor (such as California's Central Valley, the Pacific Northwest valleys, European river polders, or coastal deltas). Unlike a brief hilltop flash flood that drains away in an hour, water rushing through a broken river levee fills low-lying bowls 2 to 6 meters (6 to 20 feet) deep and cannot drain back into the river for days or weeks.
  2. If you see muddy water bubbling out of the ground behind a levee ("sand boil"), call 911 / 112 / 999 and evacuate: While clear water seeping gently through a levee is monitored, a fountain or geyser of muddy, sandy, silt-laden water bubbling up from the flat ground on the dry landward side of a levee (internal piping erosion) means water is actively tunneling out the foundation underneath the levee and a catastrophic breach can occur within minutes to hours.
  3. Never drive into water covering a road, especially near levees or culverts: Just 15 centimeters (6 inches) of fast-moving floodwater knocks an adult off their feet, 30 centimeters (12 inches) floats a compact passenger car, and 45 to 60 centimeters (18 to 24 inches) sweeps away heavy SUVs and pickup trucks. During atmospheric rivers, dark floodwater hides completely washed-out roadbeds and collapsed culverts.
  4. If floodwater rises around your home before you can drive out, move to the highest open floor or roof, never a closed attic: Shut off the main electrical circuit breaker only if you can reach the panel while standing on completely dry ground. Carry your go-bag, warm waterproof clothing, drinking water, flashlights, and a heavy axe, crowbar, or sledgehammer to the second story. Never climb into an enclosed attic unless it has a window, skylight, or gable louver large enough to climb through onto the roof, as rising water traps people against the rafters with no escape.
  5. Stay at least 10 meters (35 feet) away from steep hillsides, retaining walls, and canyon mouths: Multi-day atmospheric rivers saturate hillside soils until they liquefy into high-speed landslides and debris flows that strike downslope bedrooms without warning, particularly at night or below recent wildfire burn scars.
  6. Protect against hypothermia and sewage contamination if forced to wade: Floodwaters in winter and spring atmospheric rivers are frequently 4 to 12 degrees Celsius (39 to 54 degrees Fahrenheit) and contaminated with raw municipal sewage, pesticides, and submerged electrical currents. Wear a personal flotation device (life jacket) if you have one, use a stout pole or broom handle to probe the ground ahead of your feet for open manholes, and never touch wet electrical boxes.
flowchart TD
    Start["Category 4 or 5 Atmospheric River / Prolonged Multi-Day Basin Flood Warning"] --> Location{"1. Yeba Risque Topographique Géographique na Yo"}
    Location -->|Inside a Levee-Protected Floodplain Basin or Below a Dam| LeveeWatch["Zone ya inondation ya bassin ya bozindo ya likolo: Motuka ya carburant, Pack Go-Bag, Carte ya banzela mibale ya mabele ya likolo libanda ya bassin"]
    Location -->|Against Steep Hillsides, Bluffs, or Below Wildfire Burn Scars| SlideWatch["Debris Flow / Landslide Zone: Sleep on Upper Floor on Uphill/Side Away from Slope, Evacuate Early"]
    LeveeWatch --> BreachCheck{"2. Est-ce que Ordre ya évacuation ezali active TO Omoni ba boils ya sable ya potopoto / kokita na levee?"}
    SlideWatch --> BreachCheck
    BreachCheck -->|Yes: Breach Imminent or Ordered| EvacNow["Evacuate Immediately to High Ground Before Roads Submerge; Never Drive Through Moving Water"]
    BreachCheck -->|Trapped by Rapidly Rising Water| Vertical["3. Vertical Survival: Turn Off Main Breaker ONLY if Standing on Dry Floor, Move to Upper Story or Roof"]
    Vertical --> AtticRule["4. NEVER Enter a Closed Attic Without a Roof Window or Heavy Axe/Pry Bar to Break Through Roof Sheathing"]
    AtticRule --> Signal["5. Call 911/112/999, Wave Bright Cloth or Strobe Light from Roof/Upper Window, Stay Warm and Dry"]

The Ralph / CW3E Atmospheric River Scale (AR Cat 1 to AR Cat 5)

Developed by the Center for Western Weather and Water Extremes (CW3E) at Scripps Institution of Oceanography and adopted by the United States National Weather Service (NWS) and international hydrometeorological agencies, the Atmospheric River Scale rates storms from AR Cat 1 to AR Cat 5 based on two combined physical measurements:

  1. Maximum Integrated Vapor Transport (IVT): How much water vapor is flowing past a 1-meter-wide vertical slice of the sky every second, measured in kilograms per meter per second (\(\text{kg}\cdot\text{m}^{-1}\cdot\text{s}^{-1}\)).
  2. Duration at a single location: How many consecutive hours the atmospheric river remains aimed at the same watershed (lasting under 24 hours vs. stalling for 24 to 72+ hours).
AR Category Descriptive Rating Integrated Vapor Transport (IVT) & Duration Expected Hydrological Impact & Emergency Posture
AR Cat 1 Primarily Beneficial Weak to moderate vapor transport (250 to 500 \(\text{kg}\cdot\text{m}^{-1}\cdot\text{s}^{-1}\)) lasting 12 to 24 hours. Replenishes reservoirs and mountain snowpack with minimal flooding; localized urban street ponding in poor drainage areas.
AR Cat 2 Mostly Beneficial, Also Hazardous Moderate vapor transport (500 to 750 \(\text{kg}\cdot\text{m}^{-1}\cdot\text{s}^{-1}\)) for 12 to 24 hours, or weaker flow lasting 24 to 48 hours. Small streams and urban creeks approach bankfull; minor rockslides in steep mountain canyons; clear roof gutters and storm drains.
AR Cat 3 Balance of Beneficial and Hazardous Strong vapor transport (750 to 1,000 \(\text{kg}\cdot\text{m}^{-1}\cdot\text{s}^{-1}\)) for 24 hours, or moderate flow stalling for 48+ hours. Flood Watches and Warnings: Small rivers overflow banks; shallow mudslides on saturated slopes; high winds topple shallow-rooted trees onto power lines.
AR Cat 4 Mostly Hazardous (Extreme) Extreme vapor transport (1,000 to 1,250 \(\text{kg}\cdot\text{m}^{-1}\cdot\text{s}^{-1}\)) for 24 to 48 hours, or strong flow stalling for 48 to 72 hours. Major River Flooding and Levee Stress: Mainstem rivers surge past flood stage; reservoir emergency spillways open; widespread debris flows and road washouts; prepare for immediate basin evacuation.
AR Cat 5 Primarily Hazardous (Exceptional) Exceptional vapor transport (over 1,250 \(\text{kg}\cdot\text{m}^{-1}\cdot\text{s}^{-1}\)) stalling over the same watershed for 48 to 72+ hours (or hitting right after a previous AR Cat ¾ storm). Catastrophic Basin Inundation and Levee Failures: Historic multi-day rainfall (300 to 750+ mm / 12 to 30+ in) often combined with rapid warm rain-on-snow melt; earthen levees breach; whole towns in low basins submerge for days to weeks.

Why "Pineapple Express" and warm atmospheric rivers are twice as dangerous in winter

(Gulf of Mexico)

Instead of adding snow, warm tropical wind and heavy rain pound directly onto existing mid-elevation snowpacks (a "rain-on-snow" event). Every millimeter of rain falling across an entire mountain range, plus the rapid melting of the snowpack underneath, runs off simultaneously into the rivers, doubling or tripling peak flood volume into downstream valleys and reservoirs within 12 to 24 hours.


How earthen levees fail: overtopping, slumping, and underseepage "sand boils"

Bamilio ya bato bafandaka, basalaka bilanga, mpe basalaka na bisika ya patatalu oyo mpela ekɔtaka, na ba delta ya ebale, mpe na bisika ya bilanga to ya bingumba oyo ezindi mpe ebatelami na bankóto ya bakilomɛtrɛ ya ba levees ya mabele (ba embankments ingénierie ya mabele oyo ekangami, mabele ya lima, mpe zelo) to na bifelo ya mpela. Lokola bafandi batalaka na maninisa na bango na balabala moko ya kokauka oyo ebombami nsima ya efelo ya levee oyo ezipami na matiti, mbala mingi bazalaka na likanisi moko te ete nivo ya ebale na ngambo mosusu ya efelo wana ya bosoto ezali sikawa kosopana metele 3 kino 6 (10 kino 20 feet) likolo koleka mabele ya salon na bango, to ete leve ezali mosika na bangonga mingi mpo na kokweya nsima ya mikolo ya kozindisama.

Engebene Corps d’ingénieurs ya mampinga ya États-Unis (USACE) mpe Rijkswaterstaat (Ministère ya ba infrastructures mpe ya gestion ya mayi ya Pays-Bas), ba levees ya mabele elongi te na nzela ya ba mécanismes minei ekeseni na tango ya mayi ya likolo ya ebale oyo eumelaka mingi:

Mecanisme ya Panne ya Levee Ndenge Esalemaka Na Nzoto Bilembo ya likebisi oyo emonanaka liboso ya kobuka mobeko mobimba Ba sacs ya sable ekoki kopekisa yango?
1. Underseepage and Internal Piping ("Sand Boils") Pression ya ebale ya likolo e forcer mayi na nzela ya ba couches ya sable to ya graviers poreuses na se ya base ya levee. Lokola mai ezali kopumbwapumbwa na ngambo ya mabele oyo ekauki, ememaka mbuma ya zelo libanda uta na nse ya levee, kosala mabulu na tunnel moko ya nse ya mabele (piping) kino toit ya levee ekokwea na esika ya mpamba. A bubbling spring or volcano-shaped cone of sand (a sand boil) appearing on the flat ground or in a drainage ditch 3 to 50 meters (10 to 165 feet) inside the dry side of the levee. Yes, ONLY if the water is clear or caught early using a "Sandbag Ring" (never cover or plug a sand boil directly; build a circular chimney of sandbags around it to create counter-pressure). If a sand boil is gushing muddy/silty water rapidly, evacuate immediately.
2. Saturation Slumping (Slope Instability) After 4 to 10 days of continuous atmospheric river rain and high river levels, water saturates the earthen levee core until pore water pressure pushes the soil grains apart, turning the dry-side clay slope into mush. Mapanzani milai ya lolenge ya sanza na nzela ya motole ya likolo ya levee, oyo etombolaka na mosapi ya mopanzi ya kokauka, to eteni monene ya libongo ya matiti ya ngambo ya kokauka oyo ezali kokita na nse (ezali kokita). No: Once a saturated levee slope begins slumping, adding heavy sandbags to the top crown actually pushes the slide down faster. Evacuate immediately.
3. Through-Seepage mpe Kosukola mabulu ya banyama Burrowing animals (beavers, nutria, muskrats, ground squirrels, badgers) dig tunnels partway through the levee; high river water enters the burrow and erodes a rapidly widening pipe straight through the embankment. A jet or muddy stream of water shooting directly out of the dry-side face of the levee embankment. Requires professional flood-fight crews; rapid widening signals imminent breach.
4. Overtopping Erosion River water rises higher than the top crest of the levee and pours over the crown like a waterfall. Fast water cascading down the unprotected dry-side grass slope strips away sod and soil from the back side until the wall washes away. Water lapping within 15 to 30 centimeters (6 to 12 inches) of the top of the levee crown, or sheets of water flowing across the levee road. No for homeowners: Once water actively sheets over an earthen levee crest, it scours a 30-to-100-meter-wide gap in minutes. Evacuate immediately.

Why you must never plug a "sand boil" directly (And how engineers ring it)

If you live near a levee and discover water bubbling out of the ground on the landward side during a flood:

  1. Inspect the water clarity from a safe distance and call 911 / 112 / 999 or your local levee reclamation district immediately:
  2. Clear water seepage: If the water trickling out of the boil is crystal clear with no sand or mud, the soil skeleton underneath the levee is still intact.
  3. Muddy, cloudy, or sand-ejecting water (Active Piping Emergency): If the water is brown, muddy, or building a cone of sand grains around the hole, soil is actively being mined out from beneath the levee foundation.
  4. Never dump dirt on top of a sand boil and never step on it to plug it: Trying to seal a sand boil shut by piling sandbags directly on top of the hole blocks the pressure relief outlet; the trapped pressurized water immediately blows out a bigger, unstoppable hole two meters away or liquefies the entire levee toe.
  5. How flood-fight crews ring a sand boil (Only if trained and instructed while waiting for engineers): Flood crews build a circular ring ("chimney") of sandbags around the boil, leaving a clear water basin at least 60 to 90 centimeters (2 to 3 feet) wide around the bubbling hole. As water fills the inside of the sandbag ring and overflows gently over the top rim, the weight of the standing water column inside the ring creates downward hydrostatic back-pressure that slows the upward flow rate just enough that sand grains stop lifting out of the ground while allowing clean water to harmlessly escape.

Basin flooding versus flash flooding: why waiting to see water traps you

Residents accustomed to ordinary mbula makasi to mpe flash floods often think, "I live 3 kilometers (2 miles) away from the river levee, and even if it breaks, the water will only be ankle-deep and will drain away by tomorrow." In a levee-protected floodplain basin or polder, that assumption is fatal for three reasons:

  1. Bowl-shaped basin topography: Over centuries, natural rivers build up elevated ridges of silt along their banks (natural levees), while agricultural drainage and groundwater pumping cause the flat land miles away from the river to sink (land subsidence). As a result, the lowest part of a floodplain basin is often kilometers away from the river, sitting 3 to 8 meters (10 to 26 feet) lower than the river surface.
  2. Continuous hydraulic head through the breach: When a 100-meter-wide section of levee collapses during an AR Cat 4 or Cat 5 storm, the entire river diverts sideways through the gap like a broken dam. Even if you live 5 kilometers from the breach, a wall of water advances across the flat basin floor, submerging single-story homes up to their eaves (2.5 to 5 meters / 8 to 16 feet deep).
  3. Weeks-long ponding ("The Bathtub Effect"): Once the river finally drops days later, the billions of liters of floodwater sitting inside the sunken basin cannot flow uphill back into the river channel. The basin stays flooded like a giant bathtub for 2 to 6 weeks until engineers repair the levee break and bring in massive diesel pumps to pump the lake out.

Step-by-step survival if floodwater surrounds your home

If a levee breaches at night or an atmospheric river floods your valley before you can drive out to high ground, shift immediately from horizontal evacuation to vertical survival inside the structure:

Step 1: Immediate electrical and gas safety (Before water touches the floor)

  • Electrical main breaker rule: If the floor in front of your electrical breaker panel is 100 percent bone-dry, switch off the main breaker immediately to prevent electrical fires and electrocution as wall outlets submerge.
  • ABSOLUTE DANGER RULE: If even 1 centimeter (half an inch) of water is already standing on the floor near the electrical panel, or if your feet are wet, DO NOT enter the basement or touch the breaker box. Water conducts electricity from submerged basement wiring; stepping into a flooded basement or touching a metal breaker box while standing on a wet floor causes instant, fatal electrocution. Retreat upstairs immediately and call the utility company or emergency dispatch to disconnect power from the pole outside.
  • Propane and natural gas: Do not waste critical minutes trying to wrench a stiff outdoor gas meter if floodwater is rushing into your yard; get your family to high elevation first.

Step 2: Moving upward and avoiding the "Closed Attic Trap"

During hurricane storm surges (king tides and storm surge) and catastrophic levee breaches, one of the deadliest household mistakes is climbing up a pull-down ladder into an enclosed attic as water fills the ground floor.

Never retreat into an attic unless you have a way through the roof

When a levee breach floods a single-story house in a deep basin, water rises past the ground-floor ceiling and fills the attic space up to the roof peak. Modern residential roofs are built with 12-to-19-millimeter (half-inch to three-quarter-inch) plywood or oriented strand board (OSB) sheathing nailed onto thick rafters and covered with shingles or metal/clay tiles. A human being cannot punch, kick, or push their way through plywood roof sheathing with bare hands. Never climb into an attic unless: 1. The attic has a full-sized gable window, dormer window, or skylight that opens onto the roof, OR 2. You carry a heavy woodsman's axe, steel splitting maul, heavy sledgehammer, crowbar, or charged reciprocating saw up into the attic with you so you can chop an escape hole through the plywood sheathing between two rafters (avoiding clay tiles or solar panels if possible) before water reaches the attic floor.

Step 3: Roof survival and helicopter / boat rescue signaling

If water forces you out of an upper window onto the roof:

  1. Put on warm, waterproof layers and life jackets BEFORE going onto the roof: Atmospheric river storms bring driving rain and 60 to 110 km/h (40 to 70 mph) wind gusts at temperatures of 5 to 12 degrees Celsius (41 to 54 degrees Fahrenheit). Wet cotton clothing in a 50 km/h wind causes lethal hypothermia within 2 hours. Put on rain jackets, wool or fleece layers, hats, and heavy plastic trash bags (cut a hole for your head and arms to wear as a windproof poncho over your fleece), and put personal flotation devices (life jackets) on every child, adult, and pet.
  2. Stay near the roof peak on the leeward (downwind) side: Sit straddling or just below the ridge peak on the side sheltered from the wind, away from overhanging trees and overhead power lines that connect to the house weatherhead.
  3. Make yourself visible to rescue boats and Coast Guard / military helicopters:
  4. Tie a bright neon orange, yellow, red, or white bedsheet, tarp, or jacket securely to the chimney or vent pipe.
  5. At night, use an LED flashlight, headlamp, or smartphone flashlight flashed in sets of three (SOS: three short, three long, three short) aimed toward approaching boats or down at the roof surface (never shine a high-powered laser pointer or spotlight directly into a helicopter pilot's cockpit windshield, which blinds night-vision goggles).
  6. Call your local emergency number and report the exact number of people on the roof, their ages/medical needs, and your street address or GPS coordinates. Conserve phone battery by dimming screen brightness to minimum and closing background apps.

Vehicle survival during atmospheric rivers: culverts, sinkholes, and submerged escape

Over 60 percent of flood deaths in developed countries occur inside motor vehicles when drivers attempt to cross flooded roadways or underpasses. During an atmospheric river, driving carries two hidden hazards beyond simple water depth:

  1. Blown-out culverts and invisible road chasms: Mountain and rural roads cross hundreds of small creeks using corrugated metal pipe culverts buried beneath the asphalt. During an AR Cat 4 or Cat 5 storm, woody debris plugs the culvert entrance; water backs up behind the road embankment like a dam, saturates the roadbed, and suddenly washes out a 6-meter-deep (20-foot) canyon straight across the highway. When muddy floodwater is flowing 10 centimeters (4 inches) deep across the road surface, the water over the missing bridge or washed-out culvert looks completely flat and identical to the intact pavement, until the front wheels drop into a bottomless chasm.
  2. Nighttime railway underpasses and freeway dips: Underpasses fill with 3 to 4 meters (10 to 13 feet) of water in minutes during torrential downpours while streetlights reflect off the water surface, making the deep pool look like wet black asphalt at night.

What to do if your vehicle stalls or floats in floodwater

Follow the SWIM (Seatbelts, Windows, Out Immediately) protocol from our car in water survival guide within the first 30 to 60 seconds before the vehicle sinks below the window line:

  1. Unbuckle your seatbelt immediately and unbuckle children from oldest to youngest.
  2. Roll down or break the side window immediately (Never wait and never try to open the door): Once water rises halfway up the outside of the car door, 600+ kilograms (1,300+ pounds) of water pressure pins the door shut permanently. Press the electric window switch immediately (electric windows usually work for 10 to 60 seconds in water); if power fails, strike the lower corner of a tempered side window (never the laminated front windshield) with a spring-loaded center punch or heavy metal object.
  3. Climb out through the open window onto the roof of the car if the car is stationary in shallow water, OR swim/wade out toward the nearest high ground upstream of the current if the vehicle is being swept toward deep channel water.

Post-flood safety: returning to a basin after the water recedes

When water finally drains or is pumped out of a flooded basin days or weeks later, returning home requires strict protective precautions:

  • Check for structural foundation washout and gas leaks before entering: Walk all the way around the outside of the house first. If a corner of the foundation has settled, walls are leaning, or you smell rotten-egg natural gas (gas leak), do not enter.
  • Never start a gasoline generator indoors, in a garage, or on a porch: Post-flood carbon monoxide poisoning from portable generators placed near windows or in garages kills dozens of flood survivors after the storm passes. Keep generators at least 6 meters (20 feet) outdoors away from all doors and windows.
  • Kotala potopoto nionso ya mpela pe mayi ya kotelema lokola mayi ya bosoto ya poison ya poison: Ba bassins oyo etondi na mayi esangisaka ba lagunes ya manure agricole, ba usines ya mayi ya bosoto ya ba municipalités oyo esili kozindisama, ba fosses septiques, pe ba réservoirs ya carburant industriel. Lata ba bottes ya caoutchouc ya kilo oyo ekoki kokɔtisa mai te, ba gants ya minene ya nitrile/caoutchouc, ba lunettes, mpe respirateur N95 na tango mold and water cleanup, mpe sukola loposo nyonso oyo bakati mbala moko na sabuni mpe na mai ya pɛto ya milangi.
  • Obey Boil Water Notices and test private wells: Never drink tap water or private well water after basin flooding until your municipal water utility lifts the boil water advisory or your well has been shock-chlorinated and lab-tested for coliform bacteria and nitrates.

Mituna oyo batunaka mingi

What is an atmospheric river ("Pineapple Express"), and how is it rated from Category 1 to Category 5?

An atmospheric river is a narrow, concentrated plume of water vapor in the sky, often stretching thousands of kilometers from the tropics (such as near Hawaii in a "Pineapple Express"), that carries 7.5 to 15 times the water volume of the Mississippi River at the Gulf of Mexico. Meteorologists rate them from AR Category 1 (primarily beneficial rain) to AR Category 4 (Extreme) and AR Category 5 (Exceptional) based on the total water vapor flux and how many hours the storm stalls over a single region; Category 4 and 5 storms drop 300 to 750 millimeters (12 to 30 inches) of rain over several days, triggering catastrophic river flooding and levee failures.

What is a "sand boil" behind a levee, and why does muddy water bubbling up mean you must evacuate?

A sand boil occurs when extreme water pressure in a high river forces water through sandy soil layers underneath the base of an earthen levee, bubbling up out of the flat ground on the dry landward side. While a small trickle of crystal-clear water is monitored by engineers, a sand boil that is bubbling up brown, muddy water or building a cone of sand grains means the water is actively eroding and hollowing out an underground tunnel beneath the levee (internal piping), which can cause the entire levee wall to collapse without warning. Call emergency services and evacuate immediately, and never try to plug or dump dirt directly onto the hole.

Why is flooding from a levee breach in a valley basin much deeper and longer-lasting than a typical flash flood?

Many agricultural and urban floodplains protected by levees are shaped like giant sunken bowls that sit 3 to 8 meters (10 to 26 feet) lower than the elevated river channel. When a levee breaches, the river pours sideways into the sunken basin until water stands 2 to 6 meters (6 to 20 feet) deep over entire neighborhoods, and once the river level eventually drops, the trapped lake of floodwater cannot drain uphill back into the river, remaining for weeks until the levee is patched and giant pumps drain the basin.

Why must you never climb into a closed attic to escape rising floodwaters unless you have an axe or roof window?

In a deep levee breach or storm surge where water rises above the first-floor ceiling, climbing into an enclosed attic without an operable window, skylight, or heavy axe/pry bar traps you in an air pocket that rapidly fills to the roof peak. Because residential roofs are built with thick plywood sheathing nailed to rafters, it is physically impossible to punch or kick your way out with bare hands; always go out an upper window onto the roof instead, or carry a heavy axe into the attic so you can chop through the roof sheathing.

Why do warm winter atmospheric rivers cause much worse flooding than cold winter snowstorms?

Warm subtropical atmospheric rivers have very high freezing levels (often above 2,500 to 3,000 meters / 8,000 to 10,000 feet), meaning heavy precipitation falls as warm rain rather than snow all the way to the high mountain peaks. This triggers a "rain-on-snow" event where massive rainfall combines with rapid melting of the existing mountain snowpack, sending two to three times more runoff crashing down into reservoirs and river levees at once.


Ba sources e vérifié

  • Center for Western Weather and Water Extremes (CW3E, Scripps Institution of Oceanography) and National Oceanic and Atmospheric Administration (NOAA / National Weather Service, United States): The Ralph et al. Scale for Intensity and Impacts of Atmospheric Rivers (AR Cat 1 to AR Cat 5).
  • United States Army Corps of Engineers (USACE) and California Department of Water Resources (DWR, United States): Levee Owner's Manual for Non-Federal Flood Control Works, Underseepage Sand Boil Ringing Protocols, and Flood Fight Handbook.
  • Federal Emergency Management Agency (FEMA) and Ready.gov (United States): Floods, Levee Failure Evacuation, and Vertical Shelter Safety Guidelines.
  • Rijkswaterstaat (Ministry of Infrastructure and Water Management, Netherlands) and Environment Agency (United Kingdom): Dike and Levee Breach Inundation Modeling, Piping Erosion Recognition, and Polder Evacuation Standards.
  • United States Geological Survey (USGS): ARkStorm Megastorm Scenario and Post-Wildfire Atmospheric River Debris Flow Hazards.

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