Development and application of a modeling approach for surface water and groundwater interaction

Cho, J.; Mostaghimi, Saied; Kang, Moon‐Seong

doi:10.1016/j.agwat.2009.08.018

Cited by 26 publications

(5 citation statements)

References 21 publications

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“…However, direct demonstration of the effect of these factors on the interannual variability of winter streamflow at the seasonal scale is difficult because of the complex and diverse nature of the mechanisms that play a role in aquifer recharge (the relationship between precipitation and the amount of water infiltrating into aquifer) on the one hand and the effect of exfiltration (the relationship between aquifers and streamflow) on the other hand (Devito et al, 1996;Brunke and Gonser, 1997;Sun and Duffy, 1999;Delin et al, 2000;Halford and Mayer, 2000;Sanford, 2002;Sophocleous, 2002;de Vries and Simmers, 2002;Lambs, 2004;Rodgers et al, 2004;Vidon and Hill, 2004;Langhoff et al, 2006;Webb and Leake, 2006;Dahl et al, 2007;Brodie et al, 2008;Le Maitre and Colvin, 2008;Baskaran et al, 2009;Contor, 2009;Eslamian and Nekoueineghad, 2009;Intaraprasong and Zhan, 2009;Cho et al, 2010). For Quebec, this difficulty increases as a result of the lack of data on aquifer recharge in many catchments and the dearth of studies looking at infiltration and exfiltration mechanisms (e.g.…”

Section: Introductionmentioning

confidence: 99%

Comparison of Interannual Variability Modes and Trends of Seasonal Precipitation and Streamflow in Southern Quebec (Canada)

Assani

Landry

Laurencelle

2011

River Research & Apps

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The interactions between precipitation, streamflow and groundwater are very complex. In cold temperate regions characterized by harsh winters, winter streamflow is mainly derived from aquifers that are recharged in the spring, during snowmelt, and in the fall, when evapotranspiration is subdued. Despite this complexity, the modes and trends in the interannual variability of spring (April, May, June and July) streamflow and fall (August, September, October and November) precipitation and streamflow were compared to the modes and trends in the interannual variability of winter (December, January, February and March) streamflow in southern Quebec from 1950 to 2000. Results indicate that the variability modes are identical for all four of these hydro‐climatic variables: two modes (south‐east and east modes) on the south shore of the St. Lawrence River on either side of the 47°N and a single mode (south‐west mode) on the north shore. As for the trend, a significant increase in winter streamflow was observed on the north shore. This increase is comparable to that observed in spring streamflow, which suggests that winter streamflow on the north shore is mainly derived from groundwater recharge during the spring. Moreover, both spring and winter streamflows are positively correlated to the North Atlantic Oscillation climate index. On the south shore, south of the 47°N, a significant decrease was observed in the trend of the interannual variability of winter streamflow, this in spite of a significant increase in fall precipitation and streamflow. An increase in evaporation (decreased infiltration) due to a shift from forest cover to agricultural land cover in this region could account for this. However, fall precipitation and streamflow and winter streamflow are significantly correlated to the Atlantic Multidecadal Oscillation winter index. This correlation is negative with the first two variables but positive with the third. This study suggests that, in southern Quebec, the interannual variability of winter streamflow is mainly affected by spring recharge in non‐agricultural catchments (east and south‐west modes) and by farming in agricultural catchments (south‐east mode). Copyright © 2011 John Wiley & Sons, Ltd.

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Section: Introductionmentioning

confidence: 99%

Comparison of Interannual Variability Modes and Trends of Seasonal Precipitation and Streamflow in Southern Quebec (Canada)

Assani

Landry

Laurencelle

2011

River Research & Apps

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“…The MT3D code can be used with any finite difference flow model such as MODFLOW. MT3D paired with MODFLOW has been used in many groundwater contaminations studies (Abu-El-Sha 'r & Hatamleh, 2007;Cho et al, 2010;Eltarabily et al, 2017;Liu et al, 2011;Santos et al, 2014). The next generation of three-dimensional transport model called MT3DMS was developed by Zheng and Wang (1999) which was a significant upgrade to the MT3D.…”

Section: Reviewmentioning

confidence: 99%

Simulating contaminant transport in unsaturated and saturated groundwater zones

Sarma

Singh

2021

Water Environment Research

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The demand for clean and adequate water is rising rapidly with increasing population. This growing demand for water necessitates the measurement of the quantity and quality of water. Simulation modeling has become increasingly popular in the last two decades largely because of their predictive ability. This paper reviews the approaches for simulation modeling in groundwater resources management, focusing on models that have been used to simulate contaminant transport through the aquifer system. Recent research papers that have integrated the models for unsaturated and saturated zones have also been studied and described. Integrated models require assessment of the complex interactions between the groundwater zones and the movement of water and solute through them. Due to this, integrated models provide a more accurate modeling approach than models that have been independently developed for saturated and unsaturated zones. Application of such models is encouraged at the regional level to arrive at the best groundwater management decisions. © 2021 Water Environment Federation • Practitioner points• In the past few decades, modeling of contaminant transport in groundwater systems has seen tremendous applications. • A number of models exist that independently simulate flow and solute transport in unsaturated and saturated zones. • Recently, focus has been given on developing advanced coupled modeling approaches that require less inputs and run times.

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“…Es así que los modelos hidrológicos son representaciones simplificadas de los sistemas hidrológicos reales permiten estudiar el funcionamiento de las cuencas hidrográficas y su respuesta a diversos factores, y así obtener una mejor comprensión de los procesos hidrológicos. Estos permiten además predecir la respuesta hidrológica a varias prácticas de manejo de cuencas hidrográficas y tener una mejor comprensión de los impactos de estas prácticas (Arabi et al 2008;Cho et. al.…”

Section: Introductionunclassified

Evaluación del Sistema de Modelamiento Hidrológico HEC-HMS para la Simulación Hidrológica de una Microcuenca Andina Tropical

2019

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Se simuló el comportamiento hidrológico en una cuenca tropical en los Andes de Ecuador, conocida como la microcuenca del río Chaquilcay, en la provincia de Azuay, en Ecuador. Se obtienen hidrogramas para la determinación de caudales y para generar información hidrológica base para la gestión de cuencas, sobre todo en una zona donde no existen estudios de este tipo. Se utilizaron curvas intensidad-duración-frecuencia (IDF) para la construcción de hietogramas. Con esta información, se aplicó un sistema de modelamiento hidrológico con la herramienta HEC-HMS (versión 4.1), y el programa ArcMap 10.1 para determinar las características morfológicas de la cuenca. Se logró obtener un caudal punta en el desagüe de 1.7 m 3 /s, 1.8 m 3 /s y 1,9 m 3 /s para períodos de retorno de 25, 50 y 100 años respectivamente. Esta investigación puede ser útil para cuencas hidrográficas en el área de la región ecuatoriana, que tienen una función importante en el ecosistema y que no cuentan con información hidrometeorológica.

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Development and application of a modeling approach for surface water and groundwater interaction

Cited by 26 publications

References 21 publications

Comparison of Interannual Variability Modes and Trends of Seasonal Precipitation and Streamflow in Southern Quebec (Canada)

Comparison of Interannual Variability Modes and Trends of Seasonal Precipitation and Streamflow in Southern Quebec (Canada)

Simulating contaminant transport in unsaturated and saturated groundwater zones

Evaluación del Sistema de Modelamiento Hidrológico HEC-HMS para la Simulación Hidrológica de una Microcuenca Andina Tropical

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