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Selection: Martin:DA [3 articles] 

Publications by author Martin:DA.
 

At the nexus of fire, water and society

  
Philosophical Transactions of the Royal Society B: Biological Sciences, Vol. 371, No. 1696. (23 May 2016), 20150172, https://doi.org/10.1098/rstb.2015.0172

Abstract

The societal risks of water scarcity and water-quality impairment have received considerable attention, evidenced by recent analyses of these topics by the 2030 Water Resources Group, the United Nations and the World Economic Forum. What are the effects of fire on the predicted water scarcity and declines in water quality? Drinking water supplies for humans, the emphasis of this exploration, are derived from several land cover types, including forests, grasslands and peatlands, which are vulnerable to fire. In the last two ...

 

Current research issues related to post-wildfire runoff and erosion processes

  
Earth-Science Reviews, Vol. 122 (July 2013), pp. 10-37, https://doi.org/10.1016/j.earscirev.2013.03.004

Abstract

[Highlights] [::] Develop an organizational framework for post-wildfire response in different regions. [::] Soil properties are a critical link between infiltration, runoff, and erosion. [::] Need mathematical relations between burn severity metrics and soil properties. [::] Determine physical-based precipitation metrics that best predict runoff and erosion. [::] Incorporate basin morphology in runoff models for steep, rough channels. [Abstract] Research into post-wildfire effects began in the United States more than 70 years ago and only later extended to other parts of the world. Post-wildfire responses are typically transient, episodic, ...

 

Linking runoff response to burn severity after a wildfire

  
Hydrological Processes, Vol. 22, No. 13. (30 June 2008), pp. 2063-2074, https://doi.org/10.1002/hyp.6806
Keywords: floods   precipitation   runoff   wildfires  

Abstract

Extreme floods often follow wildfire in mountainous watersheds. However, a quantitative relation between the runoff response and burn severity at the watershed scale has not been established. Runoff response was measured as the runoff coefficient C, which is equal to the peak discharge per unit drainage area divided by the average maximum 30 min rainfall intensity during each rain storm. The magnitude of the burn severity was expressed as the change in the normalized burn ratio. A new burn severity variable, ...

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