Cover image for FLOOD HAZARD IDENTIFICATION AND MITIGATION IN SEMI- AND ARID ENVIRONMENTS.
FLOOD HAZARD IDENTIFICATION AND MITIGATION IN SEMI- AND ARID ENVIRONMENTS.
Title:
FLOOD HAZARD IDENTIFICATION AND MITIGATION IN SEMI- AND ARID ENVIRONMENTS.
Author:
French, Richard H.
ISBN:
9789814355100
Personal Author:
Physical Description:
1 online resource (237 pages)
Contents:
Contents -- Foreword -- 1. Introduction -- 1.1 Introduction -- 1.2 Alluvial Fan Hazards -- 1.3 Playa Lakes -- 1.4 Conclusion -- References -- 2. Geologic and Hydraulic Concepts of Arid Environments -- 2.1 Introduction -- 2.1.1 Desert landscape formation -- 2.2 Geologic Theories of Formative Processes -- 2.2.1 Catastrophism -- 2.2.2 Gradualism (Uniformitarianism) -- 2.2.3 Integration -- 2.3 Flow Processes -- 2.3.1 Fluvial -- 2.3.2 Hyperconcentrated flows -- 2.4 Soils -- 2.4.1 Soil formation in arid environments -- 2.4.2 Desert pavement -- 2.4.3 Indurated soil layers -- 2.4.4 Vegetation and biologic role in soil development -- 2.5 Runoff, Infiltration Potential, and Transmission Losses -- 2.5.1 Runoff and infiltration potential -- 2.5.2 Channel transmission losses -- References -- 3. Traditional Approaches to Flood Hazard Identification and Mitigation on Alluvial Fans -- 3.1 Introduction -- 3.2 Background -- 3.3 Technical Issues Regarding the Assumptions -- 3.4 Implementation of the Assumptions -- 3.4.1 Understanding the traditional approach -- 3.4.2 Implementation for hazard identification -- 3.5 An Approach to Hazard Mitigation -- 3.6 Conclusion -- References -- 4. New Approaches for Alluvial Fan Flood Hazard -- 4.1 Predicting Alluvial Fan Flooding - Background -- 4.2 FEMA's Three Phase Approach to Alluvial Fan Flood Mapping -- 4.2.1 Identification of fan geomorphology -- 4.2.2 Active versus inactive fan areas -- 4.2.3 100-year flood hazard modeling and mapping -- 4.3 Alluvial Fan Flood Modeling -- 4.3.1 Developing an alluvial fan flood model -- 4.3.2 2-D unsteady alluvial fan model limitations -- 4.3.3 Alluvial fan sediment issues -- 4.4 Important Criteria for Flood Hazard Delineation -- 4.5 Hazard Mapping as a Planning Tool -- 4.6 Flood Damage Mapping -- 4.7 Alluvial Fan Mitigation Measures -- References.

5. Flood Hazard Mapping Versus Flood Risk Analysis -- 5.1 Risk and Uncertainty of Alluvial Fan Flooding -- 5.1.1 Concepts of flood hazard and flood risk: Hazard = risk -- 5.2 Stochastic versus Deterministic Flood Hazard Assessment -- 5.3 Stochastic Methods for Fan Flood Hazards -- 5.3.1 Monte Carlo simulations -- 5.3.2 Probability distributions representing physical fan parameters -- 5.3.3 Random walk algorithm to determine flow paths -- 5.3.4 Alluvial fan flood probability - creating the linkage between the stochastic model and the deterministic model -- 5.3.5 Evolution of the alluvial fan - modeling future conditions -- 5.4 Integrating Alluvial Fan Flood Hazard Mapping and Damage Assessment -- References -- 6. Playa Lake Hazards and Resources -- 6.1 Introduction -- 6.1.1 Historic role of playas in military and civilian use -- 6.2 Inundation of Playas -- 6.2.1 Predicting the depth of inundation on playa lakes -- 6.2.2 Predicting the duration of inundation on playa lakes -- 6.3 Geologic Hazards on Playa Lakebeds -- 6.3.1 Evolution of desiccation cracks on playas -- 6.4 Playas as a Water Resource: Studies in Jordan -- 6.4.1 Azraq basin -- 6.4.2 Playas in the Northeastern Badia -- 6.4.2.1 Determining water volume on playas within the Azraq basin of Jordan -- 6.5 Conclusions -- References -- 7. Needs and Benefits of Co-Operation -- 7.1 Introduction -- 7.2 Identifying the Alluvial Fan Hydrologic Apex -- 7.3 Watershed Delineation -- 7.4 History -- 7.5 Surficial Geology -- 7.6 Paleohydrology -- 7.7 Aggradation and Scour -- 7.8 Climate Change -- 7.9 Planning -- 7.10 Summary -- References -- 8. Meeting the Challenge -- Case Study #1: Two-Dimensional Hydraulic Modeling for Alluvial Fan Floodplain Hazard Identification -- 8.1 Introduction -- 8.1.1 Local regulatory framework -- 8.1.2 Project setting -- 8.1.3 Hydraulic model development.

8.2 Hydraulic Model Data and Assumptions -- 8.2.1 Topography and grid development -- 8.2.2 Discharge -- 8.2.3 Precipitation -- 8.2.4 Infiltration -- 8.2.5 Manning's n-values -- 8.2.6 Boundary conditions -- 8.2.7 Flow obstruction -- 8.2.8 Froude number -- 8.2.9 Computational time step and grid element size -- 8.3 Hydraulic Model Results -- 8.4 Summary and Conclusions -- References -- Case Study #2: Numerical Modeling of the 2005 La Conchita Landslide, Ventura County, California -- 8.5 Introduction -- 8.6 Background, Geology, and Kinematics -- 8.6.1 Introduction -- 8.6.2 Historical setting -- 8.6.3 Geologic conditions -- 8.6.4 Vegetation and soils -- 8.6.5 Sedimentology -- 8.6.6 Physical dimensions -- 8.6.7 Velocity -- 8.7 Previous Studies of Debris Flow Behavior -- 8.8 FLO-2D Numerical Modeling -- 8.8.1 Introduction -- 8.8.2 FLO-2D modeling of debris flows -- 8.8.3 Input parameters -- 8.8.3.1 FLO-2D grid -- 8.8.3.2 Inflow hydrograph -- 8.8.3.3 Unit weight -- 8.8.3.4 Yield strength -- 8.8.3.5 Dynamic viscosity -- 8.8.3.6 Surface roughness -- 8.8.3.7 Modeling of temporary wall -- 8.8.4 Model results -- 8.8.4.1 General observations -- 8.8.4.2 Main (Eastern) lobe -- 8.8.4.3 Minor (Western) lobe -- 8.8.4.4 Channel fill -- 8.8.4.5 Sensitivity analyses -- 8.9 Summary -- References -- Case Study #3: Tiger Wash, Western Maricopa County, Arizona, USA -- 8.10 Site Description -- 8.10.1 Watershed -- 8.10.2 Geologic setting -- 8.10.3 Surficial geology -- 8.10.4 Channel morphology -- 8.10.5 Outfall -- 8.11 Flood History -- 8.11.1 Gauge record -- 8.11.2 Peak discharge estimates -- 8.11.3 September 26, 1997 flood -- 8.12 Previous Studies -- 8.13 Discussion -- 8.13.1 What is an alluvial fan? -- 8.13.2 What are the key elements of alluvial fan flooding? -- 8.13.3 Alluvial fan boundary delineation -- 8.13.4 Predicting avulsions.

8.13.5 Importance of infiltration and attenuation -- 8.13.6 Flood hazard delineation -- 8.14 Summary -- References -- 9. Future Directions -- 9.1 Introduction -- 9.2 What We Know - What We Don't Know -- 9.2.1 Education -- 9.2.2 Precipitation and flow data issues -- 9.2.3 Geology and geomorphology -- 9.2.4 Monitoring and modeling -- 9.3 Conclusion -- References.
Abstract:
Alluvial fans are ubiquitous geomorphological features that occur throughout the world, regardless of climate, at the front of mountains as the result of erosion and deposition. They are more prominent in semi- and arid climates simply because of the lack of vegetative cover that masks their fan shapes in more humid areas. From both engineering and geological viewpoints, alluvial fans present particular fluvial and sedimentation hazards in semi- and arid regions because episodic rainfall-runoff events can result in debris, mud, and fluvial flows through complex and, in some cases, migratory channel systems. Further, in semi- and arid climates alluvial fans often end in terminal or playa lakes. Given the uniform topography of playa lakes, these features often present ideal locations for facilities such as airports; however, regardless of the engineering advantages of the topography, the episodic and often long-term flooding of these lakes attracts migratory birds. The purpose of this volume is to summarize the current state-of-the-art, from the viewpoint of engineering, in the identification and mitigation of flood hazard on alluvial fans; and to accomplish this a fundamental understanding of geology is required.
Local Note:
Electronic reproduction. Ann Arbor, Michigan : ProQuest Ebook Central, 2017. Available via World Wide Web. Access may be limited to ProQuest Ebook Central affiliated libraries.
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