Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/108664
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorWeng, X-
dc.creatorZhang, B-
dc.creatorZhu, J-
dc.creatorWang, D-
dc.creatorQiu, J-
dc.date.accessioned2024-08-27T04:39:53Z-
dc.date.available2024-08-27T04:39:53Z-
dc.identifier.urihttp://hdl.handle.net/10397/108664-
dc.language.isoenen_US
dc.publisherMDPI AGen_US
dc.rights© 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Weng X, Zhang B, Zhu J, Wang D, Qiu J. Assessing Land Use and Climate Change Impacts on Soil Erosion Caused by Water in China. Sustainability. 2023; 15(10):7865 is available at https://doi.org/10.3390/su15107865.en_US
dc.subjectClimate changeen_US
dc.subjectLand use changeen_US
dc.subjectRevised universal soil loss equation (RUSLE)en_US
dc.subjectSoil erosionen_US
dc.titleAssessing land use and climate change impacts on soil erosion caused by water in Chinaen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume15-
dc.identifier.issue10-
dc.identifier.doi10.3390/su15107865-
dcterms.abstractSoil erosion poses a significant threat to land conservation, freshwater security, and ocean ecology. Climate change, with rainfall as one of its primary drivers, exacerbates this problem. Therefore, reliably predicting future soil erosion rates and taking into account anthropogenic influences are crucial for policymakers and researchers in the earth-system field. To address this challenge, we have developed a novel framework that combines the Bayesian Model Averaging (BMA) method with the Revised Universal Soil Loss Equation (RUSLE) model to estimate erosion rates on a national scale. We used BMA to merge five Regional Climate Models (RCMs), reducing uncertainty in ensemble simulations and improving the plausibility of projected changes in climatic regimes over China under two Representative Concentration Pathway (RCP) scenarios (RCP4.5 and RCP8.5). The RUSLE model was applied to forecast the effects of climate change and land-use change on water erosion in China, using high-resolution climate simulation and prediction inputs. Our findings revealed that under the RCP4.5 and RCP8.5 scenarios, average annual soil loss will increase by 21.20% and 33.06%, respectively, compared to the baseline period. Our analysis also demonstrated a clear distinction between the effects of climate change and land-use change on water erosion. Climate change leads to an increase in precipitation, which exacerbates water erosion rates, with contributions ranging from 59.99% to 78.21%. Furthermore, an increase in radiative forcing will further amplify the effects of climate change. The transformation of land from one that has not been disturbed by humans to one that has been exposed to some soil and water conservation measures will have a mitigating effect on water erosion, with a contribution of −6.96% to −4.68%. Therefore, implementing effective soil and water conservation measures can somewhat mitigate the severity of ongoing soil loss. Our findings have significant implications for policymakers seeking to develop national strategies for soil conservation and model developers working to reduce uncertainty in erosion predictions.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationSustainability, May 2023, v. 15, no. 10, 7865-
dcterms.isPartOfSustainability-
dcterms.issued2023-05-
dc.identifier.scopus2-s2.0-85160944957-
dc.identifier.eissn2071-1050-
dc.identifier.artn7865-
dc.description.validate202408 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextGuangzhou Basic and Applied Basic Research Foundation; Guangdong Natural Science Foundation; Fundamental Research Funds for the Central Universities-Sun Yat-Sen Universityen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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