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International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

Risk assessment of post-wildfire hydrological response in semiarid basins: the effects of varying rainfall representations in the KINEROS2/AGWA model

Gabriel Sidman A C , D. Phillip Guertin A , David C. Goodrich B , Carl L. Unkrich B and I. Shea Burns A
+ Author Affiliations
- Author Affiliations

A School of Natural Resources and the Environment, University of Arizona, 1311 East 4th Street, Suite 325, Tucson, AZ 85721, USA.

B Southwest Watershed Research Center, USDA-ARS, 2000 East Allen Rd, Tucson, AZ 85719, USA.

C Corresponding author. Email: gabriel.sidman@winrock.org

International Journal of Wildland Fire 25(3) 268-278 https://doi.org/10.1071/WF14071
Submitted: 2 May 2014  Accepted: 7 March 2015   Published: 7 July 2015

Abstract

Representation of precipitation is one of the most difficult aspects of modelling post-fire runoff and erosion and also one of the most sensitive input parameters to rainfall-runoff models. The impact of post-fire convective rainstorms, especially in semiarid watersheds, depends on the overlap between locations of high-intensity rainfall and areas of high-severity burns. One of the most useful applications of models in post-fire situations is risk assessment to quantify peak flow and identify areas at high risk of flooding and erosion. This study used the KINEROS2/AGWA model to compare several spatial and temporal rainfall representations of post-fire rainfall-runoff events to determine the effect of differing representations on modelled peak flow and determine at-risk locations within a watershed. Post-fire rainfall-runoff events at Zion National Park in Utah and Bandelier National Monument in New Mexico were modelled. Representations considered included both uniform and Soil Conservation Service Type II hyetographs, applying rain over the entire watershed and applying rain only on the burned area, and varying rainfall both temporally and spatially according to radar data. Results showed that rainfall representation greatly affected modelled peak flow, but did not significantly alter the model’s predictions for high-risk locations. This has important implications for post-fire assessments before a flood-inducing rainfall event, or for post-storm assessments in areas with low-gauge density or lack of radar data due to mountain beam blockage.

Additional keywords: Bandelier National Monument, design storm, peak flow, radar, rainfall representation, Zion National Park.


References

Banta RM, Barker Schaaf C (1987) Thunderstorm genesis zones in the Colorado Rocky Mountains as determined by traceback of geosynchronous satellite images. Monthly Weather Review 115, 463–476.
Thunderstorm genesis zones in the Colorado Rocky Mountains as determined by traceback of geosynchronous satellite images.Crossref | GoogleScholarGoogle Scholar |

Canfield EH, Burns IS, Goodrich DC (2005) Selection of parameters values to model post-fire runoff and sediment transport at the watershed scale in south-western forests. In ‘Watershed Management Conference Proceedings’, 19–22 July 2005, Williamsburg, VA. (Ed. GE Moglen) American Society of Civil Engineers (Williamsburg, VA)

Cannon SH, Gartner JE, Wilson RC, Bowers JC, Laber JL (2008) Storm rainfall conditions for floods and debris flows from recently burned areas in south-western Colorado and southern California. Geomorphology 96, 250–269.
Storm rainfall conditions for floods and debris flows from recently burned areas in south-western Colorado and southern California.Crossref | GoogleScholarGoogle Scholar |

Chen F, Warner TT, Manning K (2001) Sensitivity of orographic moist convection to landscape variability: a study of the Buffalo Creek, Colorado, flash flood case of 1996. Journal of the Atmospheric Sciences 58, 3204–3223.
Sensitivity of orographic moist convection to landscape variability: a study of the Buffalo Creek, Colorado, flash flood case of 1996.Crossref | GoogleScholarGoogle Scholar |

Dunkerley D (2012) Effects of rainfall intensity fluctuations on infiltration and runoff: rainfall simulation on dryland soils, Fowlers Gap, Australia. Hydrological Processes 26, 2211–2224.
Effects of rainfall intensity fluctuations on infiltration and runoff: rainfall simulation on dryland soils, Fowlers Gap, Australia.Crossref | GoogleScholarGoogle Scholar |

Faurès J, Goodrich DC, Woolhiser DA, Sorooshian S (1995) Impact of small-scale spatial rainfall variability on runoff modeling. Journal of Hydrology 173, 309–326.
Impact of small-scale spatial rainfall variability on runoff modeling.Crossref | GoogleScholarGoogle Scholar |

Foltz RB, Robichaud PR, Rhee H (2009) A synthesis of post-fire road treatments for BAER teams. USDA Forest Service, Rocky Mountain Research Station, Paper RMRS-GTR-228. (Fort Collins, CO)

Garcia M, Peters-Lidard CD, Goodrich DC (2008) Spatial interpolation of precipitation in a dense gauge network for monsoon storm events in the south-western United States. Water Resources Research 44,
Spatial interpolation of precipitation in a dense gauge network for monsoon storm events in the south-western United States.Crossref | GoogleScholarGoogle Scholar |

Goodrich DC, Faurès J, Woolhiser DA, Lane LJ, Sorooshian S (1995) Measurement and analysis of small-scale convective storm rainfall variability. Journal of Hydrology 173, 283–308.
Measurement and analysis of small-scale convective storm rainfall variability.Crossref | GoogleScholarGoogle Scholar |

Goodrich DC, Lane LJ, Shillito RM, Miller SN, Syed KH, Woolhiser DA (1997) Linearity of basin response as a function of scale in a semiarid watershed. Water Resources Research 33, 2951–2965.
Linearity of basin response as a function of scale in a semiarid watershed.Crossref | GoogleScholarGoogle Scholar |

Goodrich DC, Burns IS, Unkrich C, Semmens D, Guertin DP, Hernandez M, Yatheendradas S, Kennedy J, Levick L (2012) KINEROS2/AGWA: model use, calibration, and validation. Transactions of the ASABE 55, 1561–1574.
KINEROS2/AGWA: model use, calibration, and validation.Crossref | GoogleScholarGoogle Scholar |

Hardegree S, Van Vactor S, Healy K, Alonso C, Bonta J, Bosch D, Fisher D, Goodrich D, Harmel D, Steiner J, Van Liew M (2003) Multi-watershed evaluation of WSR-88D (NEXRAD) radar precipitation products. In ‘Proceedings of the 1st Interagency Conference on Research in the Watersheds’, 27–30 October 2003, Benson, AZ. (Eds KG Renard, S McElroy, W Gburek, E Canfield, RL Scott) USDA Agricultural Research Service, pp. 486–491. (Benson, AZ)

Hernandez M, Miller SN, Goodrich DC, Goff BF, Kepner WG, Edmonds CM, Jones KB (2000) Modeling runoff response to land-cover and rainfall spatial variability in semi-arid watersheds. In ‘Monitoring ecological condition in the western United States.’ (Eds SS Sandhu, BD Melzian, ER Long, WG Whitford, BT Walton) pp. 285–298. (Springer: New York)

Hossain F, Anagnostou EN, Dinku T, Borga M (2004) Hydrological model sensitivity to parameter and radar rainfall estimation uncertainty. Hydrological Processes 18, 3277–3291.
Hydrological model sensitivity to parameter and radar rainfall estimation uncertainty.Crossref | GoogleScholarGoogle Scholar |

Ice RL, Rhoton RD, Saxion DS, Ray CA, Patel NK, Warde DA, Free AD, Boydstun OE, Berkowitz DS, Chrisman JN, Hubbert JC, Kessinger C, Dixon M, Torres S (2007) Optimizing clutter filtering in the WSR-88D. Available at https://ams.confex.com/ams/pdfpapers/116863.pdf [Verified 19 May 2015]

Jorgensen DP, Hanshaw MN, Schmidt KM, Laber JL, Staley DM, Kean JW, Restrepo PJ (2011) Value of a dual-polarized gap-filling radar in support of southern California post-fire debris-flow warnings. Journal of Hydrometeorology 12, 1581–1595.
Value of a dual-polarized gap-filling radar in support of southern California post-fire debris-flow warnings.Crossref | GoogleScholarGoogle Scholar |

Kean JW, Staley DM, Cannon SH (2011) In situ measurements of post-fire debris flows in southern California: comparisons of the timing and magnitude of 24 debris-flow events with rainfall and soil moisture conditions. Journal of Geophysical Research: Earth Surface 116, F04019
In situ measurements of post-fire debris flows in southern California: comparisons of the timing and magnitude of 24 debris-flow events with rainfall and soil moisture conditions.Crossref | GoogleScholarGoogle Scholar |

Lambourne JJ, Stephenson D (1987) Model study of the effect of temporal storm distributions on peak discharges and volumes. Hydrological Sciences Journal 32, 215–226.
Model study of the effect of temporal storm distributions on peak discharges and volumes.Crossref | GoogleScholarGoogle Scholar |

Maddox RA, Zhang J, Gourley JJ, Howard KW (2002) Weather radar coverage over the contiguous United States. Weather and Forecasting 17, 927–934.
Weather radar coverage over the contiguous United States.Crossref | GoogleScholarGoogle Scholar |

McBean EA, Rovers FA (1998) ‘Statistical procedures for analysis of environmental monitoring data and risk assessment, Vol. 3.’ (Prentice Hall PTR: Upper Saddle River, NJ)

Milly PCD, Eagleson PS (1988) Effect of storm scale on surface runoff volume. Water Resources Research 24, 620–624.
Effect of storm scale on surface runoff volume.Crossref | GoogleScholarGoogle Scholar |

Monroe S (2012) Rito de los Frijoles – Post Las Conchas fire floods – 2011. DOI National Park Service, Bandelier National Monument. (Los Alamos, NM)

Moody JA (2011) An analytical method for predicting post-wildfire peak discharges. DOI USGS Investigations Report 2011–5236. (Reston, VA)

Moody JA, Ebel BA (2014) Infiltration and runoff generation processes in fire-affected soils. Hydrological Processes 28, 3432–3453.
Infiltration and runoff generation processes in fire-affected soils.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BC2cXls1Whtr0%3D&md5=e0fee6551ec1bf501f08cd098a6a2986CAS |

Moody JA, Martin DA (2001) Post‐fire, rainfall intensity–peak discharge relations for three mountainous watersheds in the western USA. Hydrological Processes 15, 2981–2993.
Post‐fire, rainfall intensity–peak discharge relations for three mountainous watersheds in the western USA.Crossref | GoogleScholarGoogle Scholar |

Moody JA, Martin DA (2009) Synthesis of sediment yields after wildland fire in different rainfall regimes in the western United States. International Journal of Wildland Fire 18, 96–115.
Synthesis of sediment yields after wildland fire in different rainfall regimes in the western United States.Crossref | GoogleScholarGoogle Scholar |

Moody JA, Shakesby RA, Robichaud PR, Cannon SH, Martin DA (2013) Current research issues related to post-wildfire runoff and erosion processes. Earth-Science Reviews 122, 10–37.
Current research issues related to post-wildfire runoff and erosion processes.Crossref | GoogleScholarGoogle Scholar |

Morin E, Goodrich DC, Maddox RA, Gao X, Gupta HV, Sorooshian S (2006) Spatial patterns in thunderstorm rainfall events and their coupling with watershed hydrological response. Advances in Water Resources 29, 843–860.
Spatial patterns in thunderstorm rainfall events and their coupling with watershed hydrological response.Crossref | GoogleScholarGoogle Scholar |

Muldavin E, Kennedy A, Jackson C, Neville T (2011) Vegetation classification and map – Bandelier National Monument. DOI National Park Service, Natural Resource Technical Report NPS/SCPN/NRTR 2011/438. (Fort Collins, CO)

National Oceanic and Atmospheric Administration (NOAA) (2013) NOAA Atlas 14 point precipitation frequency estimates. Available at http://hdsc.nws.noaa.gov/hdsc/pfds/pfds_map_cont.html?bkmrk=nm [Verified 18 May 2015]

National Park Service (2004) Zion National Park fire management plan: environmental assessment/assessment of effect. DOI National Park Service, Zion National Park. (Springdale, UT)

National Park Service (2006) Zion National Park fire and aviation management annual report 2006. DOI National Park Service, Zion National Park. (Springdale, UT)

National Park Service (2011) Vegetation classification and map Bandelier National Monument. DOI National Park Service, Natural Resource Technical Report NPS/SCPN/NRTR-2011/438 (Fort Collins, CO)

Natural Resources Conservation Service (2013) Web soil survey. Available at http://websoilsurvey.nrcs.usda.gov/ [Verified 18 May 2015]

Onda Y, Dietrich WE, Booker F (2008) Evolution of overland flow after a sever forest fire, Point Reyes, California. Catena 72, 13–20.
Evolution of overland flow after a sever forest fire, Point Reyes, California.Crossref | GoogleScholarGoogle Scholar |

Robichaud PR, Elliot WJ, Pierson FB, Hall DE, Moffet CA, Ashmun LE (2007) Erosion Risk Management Tool (ERMiT) user manual (version 2006.01. 18). USDA Forest Service, Rocky Mountain Research Station, General Technical Report RMRS-GTR-188. (Fort Collins, CO)

Schaffner M, Unkrich C, Goodrich D (2010) Application of the KINEROS2 site-specific model to south-central NY and north-east PA: forecasting gaged and ungaged fast-responding watersheds. National Weather Service Forecast Office, Eastern Region Technical Attachment No. 2010–01. (Binghamton, NY)

Schröter K, Llort X, Velasco-Forero C, Ostrowski M, Sempere-Torres D (2011) Implications of radar rainfall estimates uncertainty on distributed hydrological model predictions. Atmospheric Research 100, 237–245.
Implications of radar rainfall estimates uncertainty on distributed hydrological model predictions.Crossref | GoogleScholarGoogle Scholar |

Sharrow D (2012) A summary of the July 27 and August 1, 2007 Floods in Zion National Park. DOI National Park Service, Zion National Park. (Springdale, UT)

Singh VP (1998) Effect of the direction of storm movement on planar flow. Hydrological Processes 12, 147–170.
Effect of the direction of storm movement on planar flow.Crossref | GoogleScholarGoogle Scholar |

Singh VP, Woolhiser DA (2002) Mathematical modeling of watershed hydrology. Journal of Hydrologic Engineering 7, 270–292.
Mathematical modeling of watershed hydrology.Crossref | GoogleScholarGoogle Scholar |

Soil Conservation Service (SCS) (1972) ‘National engineering handbook, hydrology section. Vol. 4.’ (USDA Soil Conservation Service: Washington DC)

Stone JJ, Lane LJ, Shirley ED (1992) Infiltration and runoff simulation on a plane. Transactions of the ASABE 35, 161–170.
Infiltration and runoff simulation on a plane.Crossref | GoogleScholarGoogle Scholar |

Tao K, Barros P (2010) Using fractal downscaling of satellite precipitation products for hydrometeorological applications. Journal of Atmospheric and Oceanic Technology 27, 409–427.
Using fractal downscaling of satellite precipitation products for hydrometeorological applications.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BC3cXptVWnt70%3D&md5=256ab78528592a2ec5d18abe8d7eb731CAS |

Tillery AC, Darr MJ, Cannon SH, Michael JA (2011) Post-wildfire preliminary debris flow hazard assessment for the area burned by the 2011 Las Conchas Fire in north-central New Mexico. DOI US Geological Survey Open-File Report 2011–1308. (Reston, VA)

Tryhorn L, Lynch A, Abramson R, Parkyn K (2008) On the meteorological mechanisms driving post-fire flash floods: a case study. Monthly Weather Review 136, 1778–1791.
On the meteorological mechanisms driving post-fire flash floods: a case study.Crossref | GoogleScholarGoogle Scholar |

Woolhiser DA, Goodrich DC (1988) Effect of storm rainfall intensity patterns on surface runoff. Journal of Hydrology 102, 335–354.
Effect of storm rainfall intensity patterns on surface runoff.Crossref | GoogleScholarGoogle Scholar |

Wright DB, Smith JA, Baeck ML (2014) Critical examination of area reduction factors. Journal of Hydrologic Engineering 19, 769–776.
Critical examination of area reduction factors.Crossref | GoogleScholarGoogle Scholar |

Yatheendradas S, Wagener T, Gupta H, Unkrich C, Goodrich D, Schaffner M, Stewart A (2008) Understanding uncertainty in distributed flash flood forecasting for semiarid regions. Water Resources Research 44,
Understanding uncertainty in distributed flash flood forecasting for semiarid regions.Crossref | GoogleScholarGoogle Scholar |