Bibliographic citations
Lipa, R., Aguilar, G. (2023). Determinación de zonas de inundación mediante el análisis de dinámica fluvial del río Ramis en un tramo de 5km aguas arriba desde el puente Ramis en el distrito de Taraco [Trabajo de Suficiencia Profesional, Universidad Peruana de Ciencias Aplicadas (UPC)]. http://hdl.handle.net/10757/670237
Lipa, R., Aguilar, G. Determinación de zonas de inundación mediante el análisis de dinámica fluvial del río Ramis en un tramo de 5km aguas arriba desde el puente Ramis en el distrito de Taraco [Trabajo de Suficiencia Profesional]. PE: Universidad Peruana de Ciencias Aplicadas (UPC); 2023. http://hdl.handle.net/10757/670237
@misc{renati/409655,
title = "Determinación de zonas de inundación mediante el análisis de dinámica fluvial del río Ramis en un tramo de 5km aguas arriba desde el puente Ramis en el distrito de Taraco",
author = "Aguilar Lago, Gianmartin",
publisher = "Universidad Peruana de Ciencias Aplicadas (UPC)",
year = "2023"
}
The 5-kilometer stretch upstream from the Ramis Bridge, in the Taraco district, Huancané province, Puno department, has been the scene of recurrent floods during maximum flood events, resulting in loss of human lives, material damage, and economic losses. Therefore, the determination of critical elevations to identify flood-prone areas through hydrological modeling is the objective of this research in order to mitigate the damages. To achieve this, the thesis is divided into four secondary objectives explained as follows. First, the area under study is characterized, including general characteristics of the area, geographical and hydrographic location of the river stretch, and morphological characterization of the area using a Digital Elevation Model (DEM) obtained from the ALOS PALSAR satellite. Second, hydraulic modeling is carried out using Hec Ras software for the 5 km stretch upstream from the Ramis Bridge, including terrain elevations (DEM) and flow hydrograph data for return periods of 2, 5, 10, 50, 100, and 500 years. Third, as output data from the previous model, hydraulic flood elevations are calculated. The maximum elevations for different return periods are as follows: 1.52 m, 2.1 m, 3.79 m, 4.60 m, 5.38 m, and 5.95 m for return periods of 2, 5, 10, 50, 100, and 500 years, respectively. Finally, flood maps are generated based on the results of the fluvial dynamics analysis. The flooded areas are primarily attributed to three low-elevation points along the stretch.
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