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Nowcasting and real-time monitoring of heavy rainfall events inducing flash-floods: an application to Phlegraean area (Central-Southern Italy)

机译:令人非所决的和实时监测大雨事件诱导闪光洪水:富勒格林地区的应用(意大利南部)

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摘要

Severe weather events cause considerable disruptions to social and economic activities. Thus, high-precision meteorological products and services should be provided in order to forecast high-impacting weather conditions a few hours in advance such as those causing flash-floods. Today, this goal is mainly fulfilled by nowcasting. However, to fully comprehend alluvial phenomena, it is necessary to analyze not only the ground hydrological aspects but also the atmospheric dynamics leading to heavy precipitating events whose territorial distribution is generally complex. Herein, we analyzed the evolution of two convective storms which occurred on September 7 and 11, 2017, in the Phlegraean area (close to Naples) and explain why the first one, but not the second one, led to a flash-flood in Bacoli and Pozzuoli. We found that the traditional forecasting techniques failed since the severity of the two storms, in particular that of the first one, was not correctly forecast by Limited Area Models (LAMs). Using rainfall data, we demonstrate that LAM failed because it did not take into account the meteorological phenomenon enhancement occurring in the Phlegraean area when storms come from south-west due to the presence of Mt. Epomeo (789 m) on the nearby island of Ischia. In fact, this mountain has a quasi-pyramidal shape and is located at just 15-20 km south-west of the Phlegraean area. Thus, short/very-short time forecasting and nowcasting methodologies are not fully satisfactory. On the contrary, real-time rain-gauge monitoring networks are necessary to achieve high-safety levels in areas subject to flash-flood hazards and to promptly alert the population.
机译:恶劣的天气事件对社会和经济活动导致相当大的中断。因此,应提供高精度的气象产品和服务,以预先预测高冲击的天气条件,例如导致闪蒸洪水的那些。今天,这一目标主要是通过北卡斯特实现的。然而,为了完全理解冲积现象,不仅有必要分析地面水文方面,而且还有大气动力学,导致沉重的沉淀事件,其领土分布一般复杂。在此,我们分析了2017年9月7日和2017年9月7日和2017年9月的两种对流风暴的演变(靠近那不勒斯),并解释为什么第一个,但不是第二个,导致Bacoli的溢洪和pozzuoli。我们发现传统的预测技术因其在第一个风暴的严重程度,特别是第一个风暴的严重程度被限制面积模型(LAMS)被正确预测。利用降雨数据,我们证明林失败,因为它没有考虑到鲍尔格劳地区发生的气象现象,因为由于伊斯基亚附近的伊斯基亚附近的伊斯基亚附近岛(789米),风暴来自西南部。事实上,这座山拥有准金字塔形状,位于富勒料区西南仅15-20公里。因此,短/非常短的时间预测和漫游方法并不完全令人满意。相反,实时雨量仪监测网络是在经过闪蒸灾害的区域实现高安全水平,并迅速提醒人口。

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