Hydrological-hydrodynamic simulation and analysis of the possible influence of the wind in the extraordinary flood of 1941 in Porto Alegre

Pub Date : 2022-01-01 DOI:10.1590/2318-0331.272220220028
Thais Magalhães Possa, W. Collischonn, P. Jardim, F. Fan
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Abstract

ABSTRACT The great flood of 1941 remains the most impactful and traumatic flood event in the history of Porto Alegre. This event was caused by a combination of heavy rainfall in the basin in the days prior to the peak of the flood, and the wind that occurred during the flood. However, the influence of wind on the maximum flood level, although frequently mentioned, is not well known. This is largely because there are no systematic data for wind speed measuring and direction in 1941. Therefore, the present work aims to estimate the discharge and the maximum flood level in the city of Porto Alegre and in other relevant points of the basin. using hydrological-hydrodynamic modeling and, from there, analyze the possible role of the wind during the flood, through the simulation of hypothetical wind scenarios. The results showed that the discharges and levels were represented reasonably well with the MGB model at several locations in the basin. In relation to the 1941 event and the scenarios created, the contribution of the wind to the peak of the flood was of the order of a few to tens of centimeters, showing its potential role despite the limitations of the model.
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1941年阿雷格里港特大洪水中风可能影响的水文-水动力模拟和分析
1941年的大洪水仍然是阿雷格里港历史上影响最大、创伤最大的洪水事件。这一事件是由洪水高峰前几天盆地的强降雨和洪水期间发生的风共同造成的。然而,风对最大洪水水位的影响,虽然经常被提及,但并不为人所熟知。这主要是因为在1941年没有系统的风速测量和风向数据。因此,本工作旨在估计阿雷格里港市和流域其他相关点的流量和最大洪水位。利用水文-水动力学模型,从那里,分析风在洪水期间可能的作用,通过模拟假设的风情景。结果表明,MGB模型能较好地反映流域多个地点的流量和水位。与1941年的事件和所创造的情景相比,风对洪水峰值的贡献在几到几十厘米之间,尽管模型有局限性,但仍显示出它的潜在作用。
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