Met European Research Observatory, International Affiliates Program of the University Corporation for Atmospheric Research, Via Monte Pino snc, 82100, Benevento, Italy.
Department of History, Stockholm University, 106 91, Stockholm, Sweden.
Sci Rep. 2020 Dec 16;10(1):22062. doi: 10.1038/s41598-020-78857-3.
Rainfall erosivity and its derivative, erosivity density (ED, i.e., the erosivity per unit of rain), is a main driver of considerable environmental damages and economic losses worldwide. This study is the first to investigate the interannual variability, and return periods, of both rainfall erosivity and ED over the Mediterranean for the period 1680-2019. By capturing the relationship between seasonal rainfall, its variability, and recorded hydrological extremes in documentary data consistent with a sample (1981-2015) of detailed Revised Universal Soil Loss Erosion-based data, we show a noticeable decreasing trend of rainfall erosivity since about 1838. However, the 30-year return period of ED values indicates a positive long-term trend, in tandem with the resurgence of very wet days (> 95th percentile) and the erosive activity of rains during the past two decades. A possible fingerprint of recent warming is the occurrence of prolonged wet spells in apparently more erratic and unexpected ways.
降雨侵蚀力及其衍生指标侵蚀力密度(即单位降雨量的侵蚀力)是全球范围内造成大量环境破坏和经济损失的主要驱动因素。本研究首次调查了 1680-2019 年地中海地区降雨侵蚀力和 ED 的年际变化和重现期。通过捕捉季节性降雨及其变化与记录在案的水文极值之间的关系,这些记录在案的数据与详细的基于修订通用土壤流失方程的数据集(1981-2015 年)一致,我们表明,自大约 1838 年以来,降雨侵蚀力呈现出明显的下降趋势。然而,ED 值的 30 年重现期表明其呈正的长期趋势,这与非常湿润日(>第 95 百分位数)的重现和过去二十年来降雨的侵蚀活动同时出现。最近变暖的一个可能特征是长时间的潮湿期以更不稳定和出乎意料的方式出现。