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Towards estimates of future rainfall erosivity in Europe based on REDES and WorldClim datasets

机译:基于REDES和WorldClim数据集估算欧洲未来的降雨侵蚀力

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摘要

class="kwd-title">Keywords: R-factor, Climate change, Rainfall intensification, Storminess, RCP4.5, Erosion scenario class="head no_bottom_margin" id="ab015title">AbstractThe policy requests to develop trends in soil erosion changes can be responded developing modelling scenarios of the two most dynamic factors in soil erosion, i.e. rainfall erosivity and land cover change. The recently developed Rainfall Erosivity Database at European Scale (REDES) and a statistical approach used to spatially interpolate rainfall erosivity data have the potential to become useful knowledge to predict future rainfall erosivity based on climate scenarios. The use of a thorough statistical modelling approach (Gaussian Process Regression), with the selection of the most appropriate covariates (monthly precipitation, temperature datasets and bioclimatic layers), allowed to predict the rainfall erosivity based on climate change scenarios. The mean rainfall erosivity for the European Union and Switzerland is projected to be 857 MJ mm ha−1 h−1 yr−1 till 2050 showing a relative increase of 18% compared to baseline data (2010). The changes are heterogeneous in the European continent depending on the future projections of most erosive months (hot period: April–September). The output results report a pan-European projection of future rainfall erosivity taking into account the uncertainties of the climatic models.
机译:<!-fig ft0-> <!-fig @ position =“ anchor” mode =文章f4-> <!-fig mode =“ anchred” f5-> <!-fig / graphic | fig / alternatives / graphic mode =“ anchored” m1-> class =“ kwd-title”>关键字: R因子,气候变化,降雨加剧,暴风雨,RCP4.5,侵蚀情景类=“ head no_bottom_margin” id =“ ab015title”>摘要制定土壤侵蚀的两个最动态因素(降雨侵蚀力和土地覆盖变化)的建模方案可以响应制定土壤侵蚀变化趋势的政策要求。最近开发的欧洲规模降雨侵蚀力数据库(REDES)和用于对降雨侵蚀力数据进行空间插值的统计方法,有可能成为有用的知识,可根据气候情景预测未来的降雨侵蚀力。使用全面的统计建模方法(高斯过程回归),并选择最合适的协变量(每月降水,温度数据集和生物气候层),可以根据气候变化情景预测降雨侵蚀力。到2050年,欧洲联盟和瑞士的平均降雨侵蚀力预计为857 MJ mmha -1 h -1 yr -1 与基准数据(2010年)相比,增长了18%。在欧洲大陆,变化是不同的,具体取决于大多数侵蚀性月份(炎热期:4月至9月)的未来预测。考虑到气候模型的不确定性,输出结果报告了未来降雨侵蚀力的泛欧洲预测。

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