Results 31 to 40 of about 1,488 (141)
Abstract Understanding the factors controlling baseflow (groundwater discharge) is critical for improving streamflow predictions in the arid southwestern United States. We used an enhanced version of the Noah‐MP land surface model with advanced hydrological process options and the Routing Application for Parallel computation of Discharge (RAPID) to ...
Mohammad A. Farmani +9 more
wiley +1 more source
Abstract The interaction of groundwater (GW) and surface water (SW) not only sustains the runoff in dry seasons, but also plays an important role in regulating aquatic ecosystems. Hydrological engineers proposed the idea of modeling flood routing using the Muskingum-Cunge method.
Chengpeng Lu +8 more
openaire +1 more source
Abstract Shallow water equations (SWEs) are the backbone of most hydrodynamics models for flood prediction, river engineering, and many other water resources applications. The estimation of flow resistance, that is, the Manning's roughness coefficient n $n$, is crucial for ensuring model accuracy, and has been previously determined using empirical ...
Xiaofeng Liu, Yalan Song
wiley +1 more source
Simulation de la recharge artificielle de nappe en oued par un modèle à réservoirs [PDF]
Dans la zone semi-aride de Tunisie centrale, un grand barrage a été construit en 1982 sur l'oued Zeroud, dont l'infiltration des crues naturelles constituait jadis la principale source d'alimentation des nappes de la plaine de Kairouan.
Besbes, M., Nazoumou, Y.
core +1 more source
Accelerating River Discharge in High Mountain Asia
Abstract High Mountain Asia (HMA) plays a crucial role in Asian hydrology—its vast snow and glacier‐covered landscape significantly influences downstream river water supply for billions of people. Understanding the spatiotemporal pattern of river discharge in HMA aids effective water resource management and infrastructure planning.
J. A. Flores +23 more
wiley +1 more source
Abstract Quantitative precipitation estimation (QPE) has been an enduring challenge especially in mountainous regions due to high spatiotemporal variability of precipitation. Because of QPE uncertainty, and fast rainfall‐runoff processes in complex terrain, improvements in flood modeling through calibration of hydrologic model parameters remain elusive.
Mochi Liao, Ana P. Barros
wiley +1 more source
Assessment of different modelling studies on the spatial hydrological processes in an arid alpine catchment [PDF]
To assess the model description of spatial hydrological processes in the arid alpine catchment, SWAT and MIKE SHE were jointly applied in Yarkant River basin located in northwest China.
Bao, Anming +6 more
core +2 more sources
ABSTRACT Accurate quantification of sediment occurrence in river basins is essential for establishing sediment management strategies. This study enhanced the simplified Bagnold method within the SWAT model to enhance simulation of sediment dynamics due to the rise and fall of streamflow.
Sangjoon Bak +7 more
wiley +1 more source
Coupled surface runoff and subsurface flow model for catchment simulations [PDF]
A distributed catchment scale numerical model for the simulation of coupled surface runoff and subsurface flow is presented. Starting from rainfall (evaporation) records, the model first determines the infiltration (exfiltration) rates in the soil, by ...
Bixio, Anna Chiara +3 more
core
A novel approach for the computation of soil slope stability in distributed hydrologic applications
This paper introduces a novel methodology for the computation of slope stability at catchment scale, coupled with a hydrological model. The method improves the existing Janbu’s method of slices: a series of benchmarks are provided in order to prove that the proposed methodology outperforms the widely used Infinite Slope model.
Riccardo Bonomelli +2 more
wiley +1 more source

