Assessing the hydrologic response to wildfires in mountainous regions

This study aims to understand the hydrologic responses to wildfires in mountainous regions at various spatial scales. The Soil and Water Assessment Tool (SWAT) was used to evaluate the hydrologic responses of the upper Cache la Poudre Watershed in Colorado to the 2012 High Park and Hewlett wildfi...

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Main Authors: A. Havel, A. Tasdighi, M. Arabi
Format: Article
Language:English
Published: Copernicus Publications 2018-04-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/22/2527/2018/hess-22-2527-2018.pdf
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spelling doaj-d1e6e408176847c9bf64847a998ea4602020-11-25T01:07:43ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382018-04-01222527255010.5194/hess-22-2527-2018Assessing the hydrologic response to wildfires in mountainous regionsA. Havel0A. Havel1A. Tasdighi2A. Tasdighi3M. Arabi4Department of Civil and Environmental Engineering, Colorado State University, Fort Collins, CO 80523, USAAWR Engineering, LLC, Anchorage, AK 99519, USADepartment of Civil and Environmental Engineering, Colorado State University, Fort Collins, CO 80523, USADepartment of Civil and Environmental Engineering, University of California Irvine, Irvine, CA 92697, USADepartment of Civil and Environmental Engineering, Colorado State University, Fort Collins, CO 80523, USAThis study aims to understand the hydrologic responses to wildfires in mountainous regions at various spatial scales. The Soil and Water Assessment Tool (SWAT) was used to evaluate the hydrologic responses of the upper Cache la Poudre Watershed in Colorado to the 2012 High Park and Hewlett wildfire events. A baseline SWAT model was established to simulate the hydrology of the study area between the years 2000 and 2014. A procedure involving land use and curve number updating was implemented to assess the effects of wildfires. Application of the proposed procedure provides the ability to simulate the hydrologic response to wildfires seamlessly through mimicking the dynamic of the changes due to wildfires. The wildfire effects on curve numbers were determined comparing the probability distribution of curve numbers after calibrating the model for pre- and post-wildfire conditions. Daily calibration and testing of the model produced <q>very good</q> results. No-wildfire and wildfire scenarios were created and compared to quantify changes in average annual total runoff volume, water budgets, and full streamflow statistics at different spatial scales. At the watershed scale, wildfire conditions showed little impact on the hydrologic responses. However, a runoff increase up to 75 % was observed between the scenarios in sub-watersheds with high burn intensity. Generally, higher surface runoff and decreased subsurface flow were observed under post-wildfire conditions. Flow duration curves developed for burned sub-watersheds using full streamflow statistics showed that less frequent streamflows become greater in magnitude. A linear regression model was developed to assess the relationship between percent burned area and runoff increase in Cache la Poudre Watershed. A strong (<i>R</i><sup>2</sup>  &gt;  0.8) and significant (<i>p</i>  &lt;  0.001) positive correlation was determined between runoff increase and percentage of burned area upstream. This study showed that the effects of wildfires on hydrology of a watershed are scale-dependent. Also, using full streamflow statistics through application of flow duration curves revealed that the wildfires had a higher effect on peak flows, which may increase the risk of flash floods in post-wildfire conditions.https://www.hydrol-earth-syst-sci.net/22/2527/2018/hess-22-2527-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Havel
A. Havel
A. Tasdighi
A. Tasdighi
M. Arabi
spellingShingle A. Havel
A. Havel
A. Tasdighi
A. Tasdighi
M. Arabi
Assessing the hydrologic response to wildfires in mountainous regions
Hydrology and Earth System Sciences
author_facet A. Havel
A. Havel
A. Tasdighi
A. Tasdighi
M. Arabi
author_sort A. Havel
title Assessing the hydrologic response to wildfires in mountainous regions
title_short Assessing the hydrologic response to wildfires in mountainous regions
title_full Assessing the hydrologic response to wildfires in mountainous regions
title_fullStr Assessing the hydrologic response to wildfires in mountainous regions
title_full_unstemmed Assessing the hydrologic response to wildfires in mountainous regions
title_sort assessing the hydrologic response to wildfires in mountainous regions
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2018-04-01
description This study aims to understand the hydrologic responses to wildfires in mountainous regions at various spatial scales. The Soil and Water Assessment Tool (SWAT) was used to evaluate the hydrologic responses of the upper Cache la Poudre Watershed in Colorado to the 2012 High Park and Hewlett wildfire events. A baseline SWAT model was established to simulate the hydrology of the study area between the years 2000 and 2014. A procedure involving land use and curve number updating was implemented to assess the effects of wildfires. Application of the proposed procedure provides the ability to simulate the hydrologic response to wildfires seamlessly through mimicking the dynamic of the changes due to wildfires. The wildfire effects on curve numbers were determined comparing the probability distribution of curve numbers after calibrating the model for pre- and post-wildfire conditions. Daily calibration and testing of the model produced <q>very good</q> results. No-wildfire and wildfire scenarios were created and compared to quantify changes in average annual total runoff volume, water budgets, and full streamflow statistics at different spatial scales. At the watershed scale, wildfire conditions showed little impact on the hydrologic responses. However, a runoff increase up to 75 % was observed between the scenarios in sub-watersheds with high burn intensity. Generally, higher surface runoff and decreased subsurface flow were observed under post-wildfire conditions. Flow duration curves developed for burned sub-watersheds using full streamflow statistics showed that less frequent streamflows become greater in magnitude. A linear regression model was developed to assess the relationship between percent burned area and runoff increase in Cache la Poudre Watershed. A strong (<i>R</i><sup>2</sup>  &gt;  0.8) and significant (<i>p</i>  &lt;  0.001) positive correlation was determined between runoff increase and percentage of burned area upstream. This study showed that the effects of wildfires on hydrology of a watershed are scale-dependent. Also, using full streamflow statistics through application of flow duration curves revealed that the wildfires had a higher effect on peak flows, which may increase the risk of flash floods in post-wildfire conditions.
url https://www.hydrol-earth-syst-sci.net/22/2527/2018/hess-22-2527-2018.pdf
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