Streamflow impacts of biofuel policy-driven landscape change.

Likely changes in precipitation (P) and potential evapotranspiration (PET) resulting from policy-driven expansion of bioenergy crops in the United States are shown to create significant changes in streamflow volumes and increase water stress in the High Plains. Regional climate simulations for curre...

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Main Authors: Sami Khanal, Robert P Anex, Christopher J Anderson, Daryl E Herzmann
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2014-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC4188602?pdf=render
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spelling doaj-0d95fc1035324141ab10afe868d0990c2020-11-25T02:22:09ZengPublic Library of Science (PLoS)PLoS ONE1932-62032014-01-01910e10912910.1371/journal.pone.0109129Streamflow impacts of biofuel policy-driven landscape change.Sami KhanalRobert P AnexChristopher J AndersonDaryl E HerzmannLikely changes in precipitation (P) and potential evapotranspiration (PET) resulting from policy-driven expansion of bioenergy crops in the United States are shown to create significant changes in streamflow volumes and increase water stress in the High Plains. Regional climate simulations for current and biofuel cropping system scenarios are evaluated using the same atmospheric forcing data over the period 1979-2004 using the Weather Research Forecast (WRF) model coupled to the NOAH land surface model. PET is projected to increase under the biofuel crop production scenario. The magnitude of the mean annual increase in PET is larger than the inter-annual variability of change in PET, indicating that PET increase is a forced response to the biofuel cropping system land use. Across the conterminous U.S., the change in mean streamflow volume under the biofuel scenario is estimated to range from negative 56% to positive 20% relative to a business-as-usual baseline scenario. In Kansas and Oklahoma, annual streamflow volume is reduced by an average of 20%, and this reduction in streamflow volume is due primarily to increased PET. Predicted increase in mean annual P under the biofuel crop production scenario is lower than its inter-annual variability, indicating that additional simulations would be necessary to determine conclusively whether predicted change in P is a response to biofuel crop production. Although estimated changes in streamflow volume include the influence of P change, sensitivity results show that PET change is the significantly dominant factor causing streamflow change. Higher PET and lower streamflow due to biofuel feedstock production are likely to increase water stress in the High Plains. When pursuing sustainable biofuels policy, decision-makers should consider the impacts of feedstock production on water scarcity.http://europepmc.org/articles/PMC4188602?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Sami Khanal
Robert P Anex
Christopher J Anderson
Daryl E Herzmann
spellingShingle Sami Khanal
Robert P Anex
Christopher J Anderson
Daryl E Herzmann
Streamflow impacts of biofuel policy-driven landscape change.
PLoS ONE
author_facet Sami Khanal
Robert P Anex
Christopher J Anderson
Daryl E Herzmann
author_sort Sami Khanal
title Streamflow impacts of biofuel policy-driven landscape change.
title_short Streamflow impacts of biofuel policy-driven landscape change.
title_full Streamflow impacts of biofuel policy-driven landscape change.
title_fullStr Streamflow impacts of biofuel policy-driven landscape change.
title_full_unstemmed Streamflow impacts of biofuel policy-driven landscape change.
title_sort streamflow impacts of biofuel policy-driven landscape change.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2014-01-01
description Likely changes in precipitation (P) and potential evapotranspiration (PET) resulting from policy-driven expansion of bioenergy crops in the United States are shown to create significant changes in streamflow volumes and increase water stress in the High Plains. Regional climate simulations for current and biofuel cropping system scenarios are evaluated using the same atmospheric forcing data over the period 1979-2004 using the Weather Research Forecast (WRF) model coupled to the NOAH land surface model. PET is projected to increase under the biofuel crop production scenario. The magnitude of the mean annual increase in PET is larger than the inter-annual variability of change in PET, indicating that PET increase is a forced response to the biofuel cropping system land use. Across the conterminous U.S., the change in mean streamflow volume under the biofuel scenario is estimated to range from negative 56% to positive 20% relative to a business-as-usual baseline scenario. In Kansas and Oklahoma, annual streamflow volume is reduced by an average of 20%, and this reduction in streamflow volume is due primarily to increased PET. Predicted increase in mean annual P under the biofuel crop production scenario is lower than its inter-annual variability, indicating that additional simulations would be necessary to determine conclusively whether predicted change in P is a response to biofuel crop production. Although estimated changes in streamflow volume include the influence of P change, sensitivity results show that PET change is the significantly dominant factor causing streamflow change. Higher PET and lower streamflow due to biofuel feedstock production are likely to increase water stress in the High Plains. When pursuing sustainable biofuels policy, decision-makers should consider the impacts of feedstock production on water scarcity.
url http://europepmc.org/articles/PMC4188602?pdf=render
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