Role of surface-water and groundwater interactions on projected summertime streamflow in snow dominated regions: An integrated modeling approach

2012 ◽  
Vol 48 (11) ◽  
Author(s):  
Justin L. Huntington ◽  
Richard G. Niswonger
Water ◽  
2018 ◽  
Vol 10 (8) ◽  
pp. 1105 ◽  
Author(s):  
Yong Tian ◽  
Jianzhi Xiong ◽  
Xin He ◽  
Xuehui Pi ◽  
Shijie Jiang ◽  
...  

At the basin scale, the operation of surface water reservoirs rarely takes groundwater aquifers into consideration, which can also be regarded as reservoirs underground. This study investigates the impact of reservoir operation on the water cycle and evaluates the effect of the joint operation of surface water and groundwater reservoirs on the water conflict in arid regions through an integrated modeling approach. The Heihe River Basin (HRB) in northwestern China is selected as the study area. Our results show that the ecological operational strategies of a reservoir under construction in the upper HRB have a direct impact on the agricultural water uses and consequently affect other hydrological processes. The ecological operation strategy with a smaller water release and a longer duration is beneficial to securing the environmental flow towards the downstream area and to replenishing aquifers. With the joint operation of surface water and groundwater reservoirs, a balance among the agriculture water need, the groundwater sustainability in the Middle HRB and the ecological water need in the Lower HRB can be flexibly achieved. However, the joint operation can hardly improve the three aspects simultaneously. To resolve the water conflict in HRB, additional engineering and/or policy measures are desired.


2020 ◽  
Vol 24 (4) ◽  
pp. 1831-1858 ◽  
Author(s):  
Brian Berkowitz ◽  
Erwin Zehe

Abstract. While both surface water and groundwater hydrological systems exhibit structural, hydraulic, and chemical heterogeneity and signatures of self-organization, modelling approaches between these two “water world” communities generally remain separate and distinct. To begin to unify these water worlds, we recognize that preferential flows, in a general sense, are a manifestation of self-organization; they hinder perfect mixing within a system, due to a more “energy-efficient” and hence faster throughput of water and matter. We develop this general notion by detailing the role of preferential flow for residence times and chemical transport, as well as for energy conversions and energy dissipation associated with flows of water and mass. Our principal focus is on the role of heterogeneity and preferential flow and transport of water and chemical species. We propose, essentially, that related conceptualizations and quantitative characterizations can be unified in terms of a theory that connects these two water worlds in a dynamic framework. We discuss key features of fluid flow and chemical transport dynamics in these two systems – surface water and groundwater – and then focus on chemical transport, merging treatment of many of these dynamics in a proposed quantitative framework. We then discuss aspects of a unified treatment of surface water and groundwater systems in terms of energy and mass flows, and close with a reflection on complementary manifestations of self-organization in spatial patterns and temporal dynamic behaviour.


2019 ◽  
Author(s):  
Brian Berkowitz ◽  
Erwin Zehe

Abstract. While both surface water and groundwater hydrological systems exhibit structural, hydraulic and chemical heterogeneity, and signatures of self-organisation, modelling approaches between these two water world communities generally remain separate and distinct. To begin to unify these water worlds, we recognize that preferential flows, in a general sense, are a manifestation of self-organisation; they hinder perfect mixing within a system, due to a more energy efficient and hence faster throughput of water and matter. We develop this general notion by detailing the role of preferential flow for residence times and chemical transport, as well as for energy conversions and energy dissipation associated with flows of water and mass. Our principal focus is on the role of heterogeneity and preferential flow and transport of water and chemical species. We propose, essentially, that related conceptualizations and quantitative characterisations can be unified in terms of a theory that connects these two water worlds in a dynamic framework. We discuss key features of fluid flow and chemical transport dynamics in these two systems – surface water and groundwater – and then focus on chemical transport, merging treatment of many of these dynamics in a proposed quantitative framework. We then discuss aspects of a unified treatment of surface water and groundwater systems in terms of energy and mass flows, and close with a reflection on complementary manifestations of self-organisation in spatial patterns and temporal dynamic behaviour.


2018 ◽  
Vol 30 (3) ◽  
pp. 441-452
Author(s):  
Sha Lou ◽  
Shu-guang Liu ◽  
Gangfeng Ma ◽  
Gui-hui Zhong ◽  
Bo Li

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