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Potential impacts of climate change on soil erosion vulnerability across the conterminous United States

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Title Potential impacts of climate change on soil erosion vulnerability across the conterminous United States
Names Segura, C. (creator)
Sun, G. (creator)
McNulty, S. (creator)
Zhang, Y. (creator)
Date Issued 2014-03 (iso8601)
Note To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by the Soil and Water Conservation Society and can be found at: http://www.jswconline.org/.
Abstract Rainfall runoff erosivity (R) is one key climate factor that controls water erosion.
Quantifying the effects of climate change–induced erosivity change is important for identifying
critical regions prone to soil erosion under a changing environment. In this study
we first evaluate the changes of R from 1970 to 2090 across the United States under nine
climate conditions predicted by three general circulation models for three emissions scenarios
(A2, A1B, and B1) from the Fourth Assessment Report of the Intergovernmental Panel on
Climate Change. Then, we identify watersheds that are most vulnerable to future climate
change in terms of soil erosion potential. We develop a novel approach to evaluate future
trends of R magnitude and variance by incorporating both the rate of change with time as
well as the level of agreement between climatic projections. Our results show that mean decadal
R values would increase with time according to all nine climatic projections considered
between 1970 and 2090. However, these trends vary widely spatially. In general, catchments
in the northeastern and northwestern United States are characterized by strong increasing
trends in R, while the trends in the midwestern and southwestern United States are either
weak or inconsistent among the nine climatic projections considered. The northeastern and
northwestern United States will likely experience a significant increase in annual variability
of R (i.e., increase in extreme events). Conversely the variability of R is unlikely to change in
large areas of the Midwest. At the watershed scale (8-digit Hydrologic Unit Code), the mean
vulnerability to erosion scores vary between –0.12 and 0.35 with a mean of 0.04. The five
hydrologic regions with the highest mean vulnerability to erosion are 5, 6, 2, 1, and 17, with
values varying between 0.06 and 0.09. These regions occupy large areas of Ohio, Maryland,
Indiana, Vermont, and Illinois, with mean erosion vulnerability score statewide above 0.08.
Future watershed management aiming at reducing soil erosion should focus on areas with the
highest soil erosion vulnerability identified by this study.
Genre Article
Topic Climate change
Identifier Segura, C., Sun, G., McNulty, S., & Zhang, Y. (2014). Potential impacts of climate change on soil erosion vulnerability across the conterminous United States. Journal of Soil and Water Conservation, 69(2), 171-181. doi:10.2489/jswc.69.2.171

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