Evolution of rainfall in Italy over the last 200 years: Interactions between climate indices and global warming

IF 4.4 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES
Marco Luppichini , Monica Bini
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引用次数: 0

Abstract

This study contributes to a better understanding of past climate variability and mesoscale dynamics in the Mediterranean Basin, a region with notable sensitivity to climate change.We investigate the variations of rainfall amount and intensity by analyzing centenary time series in Italy. The study area offers an ideal setting for analyzing these dynamics due to its unique geographical position. The rainfall time series are compared to the climate indices time series to understand the influences of the mesoscale atmospheric teleconnections and of the possible changes in rainfall regimes due to an increase of the sea surface temperatures. The study is conducted by applying statistical methods on more than 100 time series. The results show that most regions of Italy have been affected by a decrease in rainfall amount and an increase in rainfall intensity over the last 200 years. This work also highlights that these patterns are correlated to positive phases of the North Atlantic Oscillation and to an increase in sea surface temperatures. The trends of climate indices thus suggest a decrease in the amount and an increase in the intensity of future rainfall distribution, with severe consequences in terms of water availability and geo-related risks.
意大利过去200年的降雨演变:气候指数与全球变暖之间的相互作用
该研究有助于更好地理解地中海盆地这一对气候变化具有显著敏感性的地区过去的气候变率和中尺度动力学。本文通过对意大利百年时间序列的分析,探讨了降雨量和降雨强度的变化。由于其独特的地理位置,该研究区域为分析这些动态提供了理想的环境。将降雨时间序列与气候指数时间序列进行比较,以了解中尺度大气遥相关的影响以及由于海面温度升高而导致的降雨状况可能发生的变化。运用统计方法对100多个时间序列进行了研究。结果表明,近200年来,意大利大部分地区都受到降雨量减少和降雨强度增加的影响。这项工作还强调,这些模式与北大西洋涛动的正相位和海面温度的升高有关。因此,气候指数的趋势表明,未来降雨分布的数量会减少,强度会增加,这在水资源供应和与地理有关的风险方面会产生严重后果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Atmospheric Research
Atmospheric Research 地学-气象与大气科学
CiteScore
9.40
自引率
10.90%
发文量
460
审稿时长
47 days
期刊介绍: The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.
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