在当前气候变化的背景下,特罗图斯特河支流上的快速洪水

IF 0.5 Q3 GEOGRAPHY
Mihaela (Tamas) Avram, M. Luca, N. Marcoie
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引用次数: 0

摘要

本文对特罗图河流域及其支流的洪水形成模式进行了分析。2004年出现了一种特殊情况,在支流上形成的洪水流量非常大,但这并没有实质性地影响主河道的流量。河流/溪流/激流型支流(例如:as、ag、Goioasa、Iedera)产生的洪水流量超出了可接受的计算概率。洪水的产生既有暴雨的作用,也有河床下部构造的作用。2004年在Trotu - pu河的一系列支流上产生的洪水,其最大流量超过了0.1%的计算概率(agagulu - 183 m3 /s, beheheet - 50.70 m3 /s, Goioasa - 67.10 m3 /s, Iedera - 127 m3 /s)。支流下游斜坡的突然变化决定了大量冲积物的沉积,这种情况减少了流段,甚至阻塞了流段。这些洪水的蔓延证实了自然和人为情况的结果,在一个有许多人类社区和重要经济活动的领土地区造成了巨大的破坏。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fast floods on the tributaries of Trotuș river, in the context of current climate change
: The paper presents an analysis of the flood formation module in the Trotu ș river basin and especially on its tributaries. A special situation was recorded in 2004 when the floods formed on the tributaries presented very high flows, but which did not substantially influence the flow of the main course. The floods produced on the river / stream / torrent type tributaries (example: Asău , Agăș , Goioasa, Iedera) presented flows that exceeded the accepted calculation probabilities. The floods produced were both the effect of torrential rainfall and the configuration of the lower sectors of the riverbeds. The floods produced in 2004 on a series of tributaries of the Trotu ș River presented maximum flows that exceeded the calculation probabilities of 0.1% ( Agăș - 183 m 3 /s, Beheghet - 50.70 m 3 /s, Goioasa - 67.10 m 3 /s, Iedera - 127 m 3 /s). The sudden change of the slope on the lower course of the tributaries determined the deposition of a large volume of alluvium, a situation that reduced the flow section and even blocked it. The result of the corroboration of natural and anthropogenic situations in the propagation of these floods is evidenced by the great destruction produced in a territorial area with numerous human communities and important economic activities.
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来源期刊
自引率
28.60%
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3
审稿时长
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