A Bayesian network to predict coastal vulnerability to sea level rise

dc.contributor.author Gutierrez, Benjamin T.
dc.contributor.author Plant, Nathaniel G.
dc.contributor.author Thieler, E. Robert
dc.date.accessioned 2011-05-17T12:59:50Z
dc.date.available 2011-05-17T12:59:50Z
dc.date.issued 2011-04-22
dc.description This paper is not subject to U.S. copyright. The definitive version was published in Journal of Geophysical Research 116 (2011): F02009, doi:10.1029/2010JF001891. en_US
dc.description.abstract Sea level rise during the 21st century will have a wide range of effects on coastal environments, human development, and infrastructure in coastal areas. The broad range of complex factors influencing coastal systems contributes to large uncertainties in predicting long-term sea level rise impacts. Here we explore and demonstrate the capabilities of a Bayesian network (BN) to predict long-term shoreline change associated with sea level rise and make quantitative assessments of prediction uncertainty. A BN is used to define relationships between driving forces, geologic constraints, and coastal response for the U.S. Atlantic coast that include observations of local rates of relative sea level rise, wave height, tide range, geomorphic classification, coastal slope, and shoreline change rate. The BN is used to make probabilistic predictions of shoreline retreat in response to different future sea level rise rates. Results demonstrate that the probability of shoreline retreat increases with higher rates of sea level rise. Where more specific information is included, the probability of shoreline change increases in a number of cases, indicating more confident predictions. A hindcast evaluation of the BN indicates that the network correctly predicts 71% of the cases. Evaluation of the results using Brier skill and log likelihood ratio scores indicates that the network provides shoreline change predictions that are better than the prior probability. Shoreline change outcomes indicating stability (−1 < rate < 1 m/yr) or erosion (rate < −1 m/yr) tend to occur for two sets of input scenarios. Stable shoreline change rates occur mainly for low rates of relative sea level rise and occur in low-vulnerability geomorphic settings. Rates indicating erosion result for cases where the rate of relative sea level rise is high and moderate-to-high vulnerability geomorphic settings occur. In contrast, accretion (rate > 1 m/yr) was not well predicted. We find that BNs can assimilate important factors contributing to coastal change in response to sea level rise and can make quantitative, probabilistic predictions that can be applied to coastal management decisions. en_US
dc.description.sponsorship Funding for this work was provided by the USGS Coastal and Marine Geology and Global Change Research programs. en_US
dc.format.mimetype application/pdf
dc.identifier.citation Journal of Geophysical Research 116 (2011): F02009 en_US
dc.identifier.doi 10.1029/2010JF001891
dc.identifier.uri https://hdl.handle.net/1912/4605
dc.language.iso en_US en_US
dc.publisher American Geophysical Union en_US
dc.relation.uri https://doi.org/10.1029/2010JF001891
dc.subject Sea level rise en_US
dc.subject Shoreline change en_US
dc.subject Bayesian networks en_US
dc.title A Bayesian network to predict coastal vulnerability to sea level rise en_US
dc.type Article en_US
dspace.entity.type Publication
relation.isAuthorOfPublication 7e1929e8-df26-476d-ad21-ab2fcc302151
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relation.isAuthorOfPublication.latestForDiscovery 7e1929e8-df26-476d-ad21-ab2fcc302151
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