Post Wildfire Flash Flood and Debris Flow Guide

Total Page:16

File Type:pdf, Size:1020Kb

Post Wildfire Flash Flood and Debris Flow Guide National Weather Service Post Wildfire Flash Flood and Debris Flow Guide Created by National Weather Service Los Angeles/Oxnard August 2015 www.weather.gov/losangeles Weather-Ready Nation Purpose of this Guide Post wildfire flash flooding and debris flows are a realistic threat in Southern California for homes and communities located within or along a wildland urban interface that has experienced a recent wildfire. It is crucial to plan and prepare for this type of hazard to prevent and reduce the loss of life and property, and to develop community resilience. The National Weather Service Office in Oxnard, CA has prepared and printed this comprehensive guide in a user-friendly manner with step-by-step guidance on what to do before, during, and after floods that could potentially follow recent wildfires. It is imperative for you to take time to develop a family disaster plan, review emergency prepara- tions and checklists regularly, build disaster supply kits in waterproof, easy-to-carry containers, and stay aware of current weather situations. Monitor statements, watches, and warnings issued by National Weather Service offices and listen to NOAA weather radio and local media broadcasts. The Emergency management community and its partners are committed to keeping Southern California residents safe when there is a threat of flash flooding and debris flows following wildland fires. We ask for your help as well by reading and studying this guide to prepare. You may also visit Weather-Ready Nation at www.nws.noaa.gov/com/weatherreadynation to learn more about NOAA’s initiative about building community resilience in the face of increasing vulnerability to extreme weather events. This guide was prepared by the National Weather Service Forecast Office in Oxnard, CA through funding provided by the NWS Advanced Hydrologic Prediction Service (AHPS). Visit us at www.weather.gov/losangeles. You can also find us on Facebook www.facebook.com/NWSLosAngeles, Twitter www.twitter.com/NWSLosAngeles, and YouTube www.youtube.com/user/NWSLosAngeles. Additional USGS information can be found at: http://landslides.usgs.gov/research/wildfire/ _______________________________________________________________________________ Los Angeles/Oxnard Weather Forecast Office NWS Los Angeles/ Oxnard, CA Southern California Post Wildfire Page 2 Flash Flood and De- 520 North Elevar Street bris Flow Guide Oxnard, California 93030 www.weather.gov/losangeles Phone: (805) 988-6610 NWS Los Angeles/Oxnard, CA Southern California Post Wildfire Page 1 Flash Flood and Debris Flow Guide Acronyms used in this Guide CA - California EAS - Emergency Activation System FEMA - Federal Emergency Management Agency NOAA - National Oceanic and Atmospheric Administration NWS - National Weather Service TADD- Turn Around Don’t Drown USGS - United States Geological Survey WEA - Weather Emergency Alert WRN - Weather-Ready Nation Front cover photo: Camarillo Springs, CA; December 12, 2014; Photo courtesy of the County of Ventura Office of Emergency Services Back cover photo: La Canada Flintridge, CA; February 6, 2010; Photo courtesy of the United States Geological Survey NWS Los Angeles/Oxnard, CA Southern California Post Wildfire Page 2 Flash Flood and Debris Flow Guide What is a Debris Flow? Before fire and rain After fire Soil is trapped on steep rocky hills by vegeta- During summer’s fire season, vegetation is tion. burned, causing sediment to roll down steep hills. Within a few hours or days, channel bottoms are loaded with loose sediment. Rain and runoff During an intense rain, the water and runoff move sediment in the steep channels, producing de- bris flows. Additional post wildfire flash flooding and debris flow web page sources: http://tinyurl.com/ye78vmw http://tinyurl.com/obvoo78 December 24, 2003 Devore, CA Debris Flow Video from the United States Geological Survey (USGS): http://tinyurl.com/nkogbel USGS Emergency Assessment of Post Debris Flow Hazards http://tinyurl.com/pezpzfe Graphics courtesy of Raoul Rañoa http://tinyurl.com/pspptm7 Copyright © 2014. Los Angeles Times. Reprinted with permission. NWS Los Angeles/Oxnard, CA Southern California Post Wildfire Page 3 Flash Flood and Debris Flow Guide Flood After Fire Fact Sheet Floods are the most common and costly natural haz- BE FLOODSMART – REDUCE YOUR RISK ard in the nation. Whether caused by heavy rain, A flood does not have to be a catastrophic event to thunderstorms, or the tropical storms, the results of bring high out-of-pocket costs, and you do not have flooding can be devastating. While some floods de- to live in a high-risk flood area to suffer flood dam- velop over time, flash floods—particularly common age. Around twenty percent of flood insurance after wildfires—can occur within minutes after the claims occur in moderate-to-low risk areas. Property onset of a rainstorm. Even areas that are not tradi- owners should remember: tionally flood-prone are at risk, due to changes to the landscape caused by fire. The Time to Prepare is Now. Gather supplies in case of a storm, strengthen your home against Residents need to protect their homes and assets damage, and review your insurance coverages. with flood insurance now—before a weather event No flood insurance? Remember: it typically takes occurs and it’s too late. 30 days for a new flood insurance policy to go WILDFIRES INCREASE THE RISK into effect, so get your policy now. You may be at an even greater risk of flooding due Only Flood Insurance Covers Flood Damage. to recent wildfires that have burned across the re- Most standard homeowner’s policies do not cov- gion. Large-scale wildfires dramatically alter the ter- er flood damage. Flood insurance is affordable. rain and ground conditions. Normally, vegetation An average flood policy costs around $600 a absorbs rainfall, reducing runoff. However, wildfires year, rates start at just $129 a year for homes in leave the ground charred, barren, and unable to ab- moderate- to low-risk areas. sorb water, creating conditions ripe for flash flooding Plan Ahead. Plan evacuation routes. Keep im- and mudflow. Flood risk remains significantly higher portant papers in a safe, waterproof place. Con- until vegetation is restored—up to 5 years after a duct a home inventory; itemize and take pictures wildfire. of possessions. Flooding after fire is often more severe, as debris Everyone is at risk for spring flooding, yet many re- and ash left from the fire can form mudflows. As main unprotected. Just a few inches of water can rainwater moves across charred and denuded cause tens of thousands of dollars in damage. The ground, it can also pick up soil and sediment and average flood claim in 2010 was approximately carry it in a stream of floodwaters. These mudflows $28,000, and without flood insurance, many must can cause significant damage. cover the costs to repair or rebuild on their own. For example, in June 2011, the Las Conchas Wild- Residents should consider their risk and the conse- fire charred more than 150,000 acres in New Mexi- quences of a flood event, and make the choice to co. One month later, heavy rains flooded the burn protect themselves. area, prompting a Presidential Disaster Declaration. Visit FloodSmart.gov (or call 1-800-427-2419) to learn more about individual flood risk, explore cover- age options and to find an agent in your area. NWS Los Angeles/Oxnard, CA Southern California Post Wildfire Page 4 Flash Flood and Debris Flow Guide Flood After Fire Risks Floods are the number 1 natural disaster in the almost anywhere, but the most commonly af- United States. Flooding causes damage and fected states are Arizona, California, Idaho, Ne- destruction across all regions, wiping out vada, Oregon, and Washington. homes and businesses. However, many resi- Heavy Rains dents and business owners are unaware that they qualify for flood insurance. You can take Excessive amounts of rainfall can happen steps to reduce the financial impact of flooding throughout the year, putting your property at before disaster strikes. risk. Properties directly affected by fires and those located below or downstream of burn are- One important step is understanding your risk. as are most at risk for flooding. Wildfires dramatically change landscape and ground conditions, which can lead to increased Flash Floods risk of flooding due to heavy rains, flash flood- A flash flood is a rapid flooding of low-lying are- ing, and mudflows. as in less than 6 hours, which can be caused Residents and business owners are urged to by intense rainfall. Flash floods are known to purchase flood insurance now to guarantee fi- roll boulders, tear out trees, and destroy build- nancial protection from flooding. There typically ings and bridges. is a 30-day waiting period before flood insur- Mudflows ance takes effect. But the Biggert-Waters Flood Mudflows are rivers of liquid and flowing mud Insurance Reform Act of 2012 allows for an ex- on the surface of normally dry land, often ception to the waiting period in certain cases caused by a combination of brush loss and sub- where property is affected by flooding on sequent heavy rains. Mudflows can develop burned Federal land that is a result of, or is ex- when water saturates the ground, such as from acerbated by, post-wildfire conditions. For more rapid snowmelt or heavy or long periods of rain- information, please contact your insurance fall, causing a thick, liquid, downhill flow of agent. earth. Mudflows are covered by flood insurance Flood after Fire: The Risks but are different from other non-covered earth You may be at an even greater risk of flooding movements where there is not a flowing char- after a wildfire. Normally, vegetation absorbs acteristic—such as landslides or slope failures. rainfall, reducing runoff. However, wildfires leave the ground charred, barren, and unable to To learn more about your risk for flooding and absorb water, creating conditions ripe for flash how to prepare for floods, visit flooding and mudflow.
Recommended publications
  • Module III – Fire Analysis Fire Fundamentals: Definitions
    Module III – Fire Analysis Fire Fundamentals: Definitions Joint EPRI/NRC-RES Fire PRA Workshop August 21-25, 2017 A Collaboration of the Electric Power Research Institute (EPRI) & U.S. NRC Office of Nuclear Regulatory Research (RES) What is a Fire? .Fire: – destructive burning as manifested by any or all of the following: light, flame, heat, smoke (ASTM E176) – the rapid oxidation of a material in the chemical process of combustion, releasing heat, light, and various reaction products. (National Wildfire Coordinating Group) – the phenomenon of combustion manifested in light, flame, and heat (Merriam-Webster) – Combustion is an exothermic, self-sustaining reaction involving a solid, liquid, and/or gas-phase fuel (NFPA FP Handbook) 2 What is a Fire? . Fire Triangle – hasn’t change much… . Fire requires presence of: – Material that can burn (fuel) – Oxygen (generally from air) – Energy (initial ignition source and sustaining thermal feedback) . Ignition source can be a spark, short in an electrical device, welder’s torch, cutting slag, hot pipe, hot manifold, cigarette, … 3 Materials that May Burn .Materials that can burn are generally categorized by: – Ease of ignition (ignition temperature or flash point) . Flammable materials are relatively easy to ignite, lower flash point (e.g., gasoline) . Combustible materials burn but are more difficult to ignite, higher flash point, more energy needed(e.g., wood, diesel fuel) . Non-Combustible materials will not burn under normal conditions (e.g., granite, silica…) – State of the fuel . Solid (wood, electrical cable insulation) . Liquid (diesel fuel) . Gaseous (hydrogen) 4 Combustion Process .Combustion process involves . – An ignition source comes into contact and heats up the material – Material vaporizes and mixes up with the oxygen in the air and ignites – Exothermic reaction generates additional energy that heats the material, that vaporizes more, that reacts with the air, etc.
    [Show full text]
  • Overview of Landslide Hydrology
    water Editorial Overview of Landslide Hydrology Roy C. Sidle 1,2,* , Roberto Greco 3 and Thom Bogaard 4 1 Mountain Societies Research Institute, University of Central Asia, Khorog GBAO 736000, Tajikistan 2 Sustainability Research Centre, University of the Sunshine Coast, 90 Sippy Downs Dr., Sippy Downs 4556, Queensland, Australia 3 Dipartimento di Ingegneria, Università degli Studi della Campania ‘L. Vanvitelli’, via Roma 9, 81031 Aversa (CE), Italy; [email protected] 4 Department of Water Management, Delft University of Technology, PO Box 5048, 2600 GA Delft, The Netherlands; [email protected] * Correspondence: [email protected]; Tel.: +996-770-822-144 Received: 11 January 2019; Accepted: 15 January 2019; Published: 16 January 2019 Most landslides and debris flows worldwide occur during or following periods of rainfall, and many of these have been associated with major disasters causing extensive property damage and loss of life [1–9]. Given concerns about the effects of climate change on precipitation regime, in the future, some mountainous areas may likely experience more landslides with a faster response to rainfall; however, most such projections are weakly based and remain untested [10,11]. Subsurface hydrology is usually the main triggering mechanism of these landslides and associated debris flows. While the effects of hillslope hydrology on runoff generation have been thoroughly studied, much less attention has been paid to these effects on landslide and debris flow initiation. Recent syntheses demonstrate that it is no longer appropriate to view the subsurface as a static media which facilitates the transit of subsurface water, rather a variety of factors affecting the dynamics of subsurface hydrology need to be considered [12,13].
    [Show full text]
  • Hazard Identification and Vulnerability Analysis Revised January 2016
    COMPREHENSIVE EMERGENCY HAZARD IDENTIFICATION MANAGEMENT PLAN AND VULNERABILITY ANALYSIS CITY OF OLYMPIA, WASHINGTON HAZARD IDENTIFICATION AND VULNERABILITY ANALYSIS REVISED JANUARY 2016 OLYMPIA FIRE DEPARTMENT, EMERGENCY MANAGEMENT DIVISION 100 EASTSIDE STREET, N. E., OLYMPIA, WA 98506 JANUARY 2016 PAGE 1 OF 48 COMPREHENSIVE EMERGENCY HAZARD IDENTIFICATION MANAGEMENT PLAN AND VULNERABILITY ANALYSIS THIS PAGE LEFT INTENTIONALLY BLANK. JANUARY 2016 PAGE 2 OF 48 COMPREHENSIVE EMERGENCY HAZARD IDENTIFICATION MANAGEMENT PLAN AND VULNERABILITY ANALYSIS EXECUTIVE SUMMARY The Hazard Identification and Vulnerability Analysis (HIVA) for the City of Olympia identifies various hazards in the region and then assesses the risk associated with each hazard. The City of Olympia Comprehensive Emergency Management Plan, which facilitates each phase of emergency management, is built upon and designed to coordinate with this HIVA in accordance with WAC 118-30-060 (1) which states, “Each political subdivision must base its Comprehensive Emergency Management Plan on a hazard analysis.” This HIVA serves as a foundation for city planning including preparedness, mitigation, response, and recovery activities and is a training tool, providing introductory knowledge of the hazards in City of Olympia. The data contained within the HIVA is not original, but extracted from many sources. The HIVA assesses potential hazards within the city, and surrounding areas with a focus on hazards that have the potential to cause large-scale disasters as well as hazards with less severe impacts that still require significant planning and response efforts to mitigate or neutralize. Even if the City of Olympia is not directly impacted by a hazard there is still a potential for significant indirect impact on the city as various critical infrastructure systems owned, operated, or utilized by the City extend beyond its borders.
    [Show full text]
  • Flood After Fire Fact Sheet: Risks and Protection
    FACT SHEET Flood After Fire Fact Sheet Risks and Protection Floods are the most common and costly natural hazard in the nation. Whether caused by heavy rain, BE FLOODSMART – REDUCE YOUR RISK thunderstorms, or the tropical storms, the results of A flood does not have to be a catastrophic event to flooding can be devastating. While some floods develop bring high out-of-pocket costs, and you do not have over time, flash floods—particularly common after to live in a high-risk flood area to suffer flood wildfires—can occur within minutes after the onset of a damage. Around twenty percent of flood insurance rainstorm. Even areas that are not traditionally flood- claims occur in moderate-to-low risk areas. Property prone are at risk, due to changes to the landscape owners should remember: caused by fire. The Time to Prepare is Now. Gather supplies in Residents need to protect their homes and assets with case of a storm, strengthen your home against flood insurance now—before a weather event occurs damage, and review your insurance coverages. and it’s too late. No flood insurance? Remember: it typically takes 30 days for a new flood insurance policy to go WILDFIRES INCREASE THE RISK into effect, so get your policy now. You may be at an even greater risk of flooding due to . Only Flood Insurance Covers Flood Damage. recent wildfires that have burned across the region. Most standard homeowner’s policies do not cover Large-scale wildfires dramatically alter the terrain and flood damage. Flood insurance is affordable. An ground conditions.
    [Show full text]
  • Fire Service Features of Buildings and Fire Protection Systems
    Fire Service Features of Buildings and Fire Protection Systems OSHA 3256-09R 2015 Occupational Safety and Health Act of 1970 “To assure safe and healthful working conditions for working men and women; by authorizing enforcement of the standards developed under the Act; by assisting and encouraging the States in their efforts to assure safe and healthful working conditions; by providing for research, information, education, and training in the field of occupational safety and health.” This publication provides a general overview of a particular standards- related topic. This publication does not alter or determine compliance responsibilities which are set forth in OSHA standards and the Occupational Safety and Health Act. Moreover, because interpretations and enforcement policy may change over time, for additional guidance on OSHA compliance requirements the reader should consult current administrative interpretations and decisions by the Occupational Safety and Health Review Commission and the courts. Material contained in this publication is in the public domain and may be reproduced, fully or partially, without permission. Source credit is requested but not required. This information will be made available to sensory-impaired individuals upon request. Voice phone: (202) 693-1999; teletypewriter (TTY) number: 1-877-889-5627. This guidance document is not a standard or regulation, and it creates no new legal obligations. It contains recommendations as well as descriptions of mandatory safety and health standards. The recommendations are advisory in nature, informational in content, and are intended to assist employers in providing a safe and healthful workplace. The Occupational Safety and Health Act requires employers to comply with safety and health standards and regulations promulgated by OSHA or by a state with an OSHA-approved state plan.
    [Show full text]
  • Documentation and Analysis of Flash Flood Prone Streams and Subwatershed Basins in Pulaski County, Virginia
    DOCUMENTATION AND ANALYSIS OF FLASH FLOOD PRONE STREAMS AND SUBWATERSHED BASINS IN PULASKI COUNTY, VIRGINIA Prepared by Anthony Phillips Department of Geography Virginia Polytechnic Institute & State University Report Distributed August 10, 2009 Prepared for National Oceanic and Atmospheric Administration - National Weather Service Blacksburg, Virginia & Office of the Emergency Manager Pulaski County, Virginia The research on which this report is based was financed by Virginia Tech through the McNair Scholars Summer Research Program. ABSTRACT Flash flooding is the number one weather-related killer in the United States. With so many deaths related to this type of severe weather, additional detailed information about local streams and creeks could help forecasters issue more accurate and precise warnings, which could help save lives. Using GIS software, streams within twenty-five feet of a roadway in Pulaski County, Virginia were identified and selected to be surveyed. Field work at each survey point involved taking measurements to determine the required stream level rise necessary to cause flooding along any nearby roadway(s). Additionally, digital pictures were taken to document the environment upstream and downstream at each survey point. This information has been color- coded, mapped, and overlaid in Google Earth for quick access on computers at the National Weather Service Office in Blacksburg, Virginia. It has also been compiled into an operational handbook and DVD for use at the NWS. iii ACKNOWLEDGMENTS The author would like to thank
    [Show full text]
  • Types of Flooding
    Designed for safer living® Focus on Types of flooding Designed for safer living® is a program endorsed by Canada’s insurers to promote disaster-resilient homes. About the Institute for Catastrophic Loss Reduction The Institute for Catastrophic Loss Reduction (ICLR), established in 1997, is a world-class centre for multidisciplinary disaster prevention research and communication. ICLR is an independent, not-for-profit research institute founded by the insurance industry and affiliated with Western University, London, Ontario. The Institute’s mission is to reduce the loss of life and property caused by severe weather and earthquakes through the identification and support of sustained actions that improve society’s capacity to adapt to, anticipate, mitigate, withstand and recover from natural disasters. ICLR’s mandate is to confront the alarming increase in losses caused by natural disasters and to work to reduce deaths, injuries and property damage. Disaster damage has been doubling every five to seven years since the 1960s, an alarming trend. The greatest tragedy is that many disaster losses are preventable. ICLR is committed to the development and communication of disaster prevention knowledge. For the individual homeowner, this translates into the identification of natural hazards that threaten them and their home. The Institute further informs individual homeowners about steps that can be taken to better protect their family and their homes. Waiver The content of this publication is to be used as general information only. This publication does not replace advice from professionals. Contact a professional if you have questions about specific issues. Also contact your municipal government for information specific to your area.
    [Show full text]
  • Effects of Sediment Pulses on Channel Morphology in a Gravel-Bed River
    Effects of sediment pulses on channel morphology in a gravel-bed river Daniel F. Hoffman† Emmanuel J. Gabet‡ Department of Geosciences, University of Montana, Missoula, Montana 59802, USA ABSTRACT available to it. The delivery of sediment to riv- channel widening, braiding, and fi ning of bed ers and streams in mountain drainage basins material, followed by coarsening, construction Sediment delivery to stream channels in often comes in large, infrequent pulses from of coarse grained terraces, and formation of mountainous basins is strongly episodic, landslides and debris fl ows (Benda and Dunne, new side channels. After the sediment wave had with large pulses of sediment typically 1997; Gabet and Dunne, 2003). This sediment passed, they observed channel incision down to delivered by infrequent landslides and debris supply regime differs from that of channels an immobile bed and bedrock. Cui et al. (2003) fl ows. Identifying the role of large but rare in lowland environments with a more regular conducted fl ume experiments to investigate sed- sediment delivery events in the evolution of sediment supply and is refl ected in the form iment pulses and found that in a channel with channel morphology and fl uvial sediment and textural composition of the channel and alternate bars, the bed relief decreased with the transport is crucial to an understanding of fl oodplain. Processing large pulses of sediment arrival of the downstream edge of the sediment the development of mountain basins. In July can be slow and leave a lasting legacy on the wave, and increased as the upstream edge of the 2001, intense rainfall triggered numerous valley fl oor.
    [Show full text]
  • Flash Flood PREPAREDNESS
    Flash Flood PREPAREDNESS Flash floods occur within a few minutes or Before a flood occurs. hours of excessive rainfall, a dam or levee failure or a sudden release of water held by an Find out if you live in a flood prone area. ice jam. Flash floods can roll boulders, tear out You can check with your local building trees, destroy buildings and bridges. Flash department to see the flood maps for your floods can also trigger catastrophic mudslides. municipality. Flash floods are the #1 weather related killer If you are in a flood zone - purchase in the United States. sufficient flood insurance. Flood losses are not covered under normal National Weather Service . homeowner’s insurance. Staying current with forecasts from the Learn how your community would alert you National Weather Service can be an important if a flood was occurring or predicted. part of flood preparedness. Individuals can purchase a NOAA weather radio to directly Pre-assemble flood-fighting supplies like hear the forecasts, advisories, watches and/or plastic sheeting, lumber, sandbags. warnings. Some NOAA weather radios can alarm when there is a serious/dangerous Have check valves installed in building weather condition. These radios are available sewer traps to prevent flood waters from at many stores. backing up in sewer drains. The following terms may be used by the As a last resort have large corks or National Weather service: stoppers to plug showers, tubs or basins from water rising up through the pipes. A Flash Flood or Flood Watch means that flash flooding or flooding is possible within the Maintain a disaster supply kit at home.
    [Show full text]
  • Disaster Management of India
    DISASTER MANAGEMENT IN INDIA DISASTER MANAGEMENT 2011 This book has been prepared under the GoI-UNDP Disaster Risk Reduction Programme (2009-2012) DISASTER MANAGEMENT IN INDIA Ministry of Home Affairs Government of India c Disaster Management in India e ACKNOWLEDGEMENT The perception about disaster and its management has undergone a change following the enactment of the Disaster Management Act, 2005. The definition of disaster is now all encompassing, which includes not only the events emanating from natural and man-made causes, but even those events which are caused by accident or negligence. There was a long felt need to capture information about all such events occurring across the sectors and efforts made to mitigate them in the country and to collate them at one place in a global perspective. This book has been an effort towards realising this thought. This book in the present format is the outcome of the in-house compilation and analysis of information relating to disasters and their management gathered from different sources (domestic as well as the UN and other such agencies). All the three Directors in the Disaster Management Division, namely Shri J.P. Misra, Shri Dev Kumar and Shri Sanjay Agarwal have contributed inputs to this Book relating to their sectors. Support extended by Prof. Santosh Kumar, Shri R.K. Mall, former faculty and Shri Arun Sahdeo from NIDM have been very valuable in preparing an overview of the book. This book would have been impossible without the active support, suggestions and inputs of Dr. J. Radhakrishnan, Assistant Country Director (DM Unit), UNDP, New Delhi and the members of the UNDP Disaster Management Team including Shri Arvind Sinha, Consultant, UNDP.
    [Show full text]
  • Bedload Transport and Large Organic Debris in Steep Mountain Streams in Forested Watersheds on the Olympic Penisula, Washington
    77 TFW-SH7-94-001 Bedload Transport and Large Organic Debris in Steep Mountain Streams in Forested Watersheds on the Olympic Penisula, Washington Final Report By Matthew O’Connor and R. Dennis Harr October 1994 BEDLOAD TRANSPORT AND LARGE ORGANIC DEBRIS IN STEEP MOUNTAIN STREAMS IN FORESTED WATERSHEDS ON THE OLYMPIC PENINSULA, WASHINGTON FINAL REPORT Submitted by Matthew O’Connor College of Forest Resources, AR-10 University of Washington Seattle, WA 98195 and R. Dennis Harr Research Hydrologist USDA Forest Service Pacific Northwest Research Station and Professor, College of Forest Resources University of Washington Seattle, WA 98195 to Timber/Fish/Wildlife Sediment, Hydrology and Mass Wasting Steering Committee and State of Washington Department of Natural Resources October 31, 1994 TABLE OF CONTENTS LIST OF FIGURES iv LIST OF TABLES vi ACKNOWLEDGEMENTS vii OVERVIEW 1 INTRODUCTION 2 BACKGROUND 3 Sediment Routing in Low-Order Channels 3 Timber/Fish/Wildlife Literature Review of Sediment Dynamics in Low-order Streams 5 Conceptual Model of Bedload Routing 6 Effects of Timber Harvest on LOD Accumulation Rates 8 MONITORING SEDIMENT TRANSPORT IN LOW-ORDER CHANNELS 11 Monitoring Objectives 11 Field Sites for Monitoring Program 12 BEDLOAD TRANSPORT MODEL 16 Model Overview 16 Stochastic Model Outputs from Predictive Relationships 17 24-Hour Precipitation 17 Synthesis of Frequency of Threshold 24-Hour Precipitation 18 Peak Discharge as a Function of 24-Hour Precipitation 21 Excess Unit Stream Power as a Function of Peak Discharge 28 Mean Scour
    [Show full text]
  • Severe Weather Safety Guide Flash Flooding
    What causes River Flooding? Stay informed! • Persistent storms over the same area for long Listen to NOAA Weather Radio, local radio or Severe periods of time. television for the latest weather and river forecasts. • Combined rainfall and snowmelt • Ice jams Weather • Releases from man made lakes • Excessive rain from tropical systems making Safety landfall. How does the NWS issue To check out the latest river forecast information Guide and current stages on our area rivers, visit: Flood/Flash Flood Warnings? http://weather.gov/pah/ahps Flash Check out the National Weather Service Paducah website for the latest information at Flooding weather.gov/paducah Call for the latest forecast from the National Weather Service’s Weather Information Now number: Paducah, KY: 270-744-6331 Evansville, IN: 812-425-5549 National Weather Service forecasters rely on a A reference guide from your network of almost 10,000 gages to monitor the National Oceanic & Atmospheric Administration height of rivers and streams across the Nation. National Weather Service National Weather Service This gage data is only one of many different 8250 Kentucky Highway 3520 Paducah, Kentucky sources for data. Forecasters use data from the Doppler Radar, surface weather observations, West Paducah, KY 42086 snow melt/cover information and many other 270-744-6440 different data sources in order to monitor the threat for flooding. FLOODS KILL MORE PEOPLE FACT: Almost half of all flash flood Flooding PER YEAR THAN ANY OTHER fatalities occur in vehicles. WEATHER PHENOMENAN. fatalities occur in vehicles. Safety • As little as 6 inches of water may cause you to lose What are Flash Floods ? control of your vehicle.
    [Show full text]