Geoestudios, Casilla 123 Puente Alto, Santiago, Chile 3 Centro de Investigación Gaia Antártica (CIGA), Universidad de Magallanes, Casilla 113, Punta Arenas, Chile 4 Scientific Department, Chilean Antarctic Institute, Punta Arenas, Chile
Geoestudios, Casilla 123 Puente Alto, Santiago, Chile 3 Centro de Investigación Gaia Antártica (CIGA), Universidad de Magallanes, Casilla 113, Punta Arenas, Chile 4 Scientific Department, Chilean Antarctic Institute, Punta Arenas, Chile
Faculty of Medicine, School of Medicine, Universidad de Chile, Santiago 8380456, Chile 3 Cardiovascular Research Unit, Hospital Clínico Universidad de Chile, Santiago 8380456, Chile * Author to whom correspondence should be addressed. Diagnostics 2024, 14(9), 893; https://doi.org/10.3390/diagnosti...
(in advance and recession), the hypsometric curve, the hydrographs, the flood peak times, the soil erosion, and consequently the runoff estimates and the flow design that support the waterworks safety. At the sub-basin scale, the effects of slopes on hillsides and channels propagate in ...