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The 20 February 2010 Madeira flash-floods: synoptic analysis and extreme rainfall assessment

机译:2010年2月20日Guckira Flash-Floods:天气分析和极端降雨评估

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This study aims to characterise the rainfall exceptionality and the meteorological context of the 20 February 2010 flash-floods in Madeira (Portugal). Daily and hourly precipitation records from the available rain-gauge station networks are evaluated in order to reconstitute the temporal evolution of the rainstorm, as its geographic incidence, contributing to understand the flash-flood dynamics and the type and spatial distribution of the associated impacts. The exceptionality of the rainstorm is further confirmed by the return period associated with the daily precipitation registered at the two long-term record stations, with 146.9 mm observed in the city of Funchal and 333.8 mm on the mountain top, corresponding to an estimated return period of approximately 290 yr and 90 yr, respectively. Furthermore, the synoptic associated situation responsible for the flash-floods is analysed using different sources of information, e.g., weather charts, reanalysis data, Meteosat images and radiosounding data, with the focus on two main issues: (1) the dynamical conditions that promoted such anomalous humidity availability over the Madeira region on 20 February 2010 and (2) the uplift mechanism that induced deep convection activity.
机译:本研究旨在将2010年2月20日闪蒸(葡萄牙)的降雨异常和气象背景的性能和气象背景。从可用的雨量速率站网络进行日常和每小时​​降水记录,以重建暴雨的时间演变,因为其地理发生率,有助于了解闪光动态以及相关影响的类型和空间分布。通过与两种长期记录站登录的日常降水相关的返回期进一步证实了暴雨的异常性,在Funchal市观察到146.9毫米,山顶上333.8毫米,对应估计的回报期大约290毫克和90年。此外,使用不同的信息来源,例如天气图,再分析数据,Meteosat图像和放射数据,分析负责闪现溢洪的概要相关情况,重点是两个主要问题:(1)促进的动态条件在2010年2月20日和(2)诱导深对流活动的隆起机制上的这种异常湿度可用性。

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