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Marco Delle Rose, Corrado Fidelibus and Paolo Martano
In this note, the Water Budget Method (WBM) is applied to estimate local values of the specific yield of the deep karst aquifer of Salento peninsula. A selection in a period of two years of relevant short precipitation events has been considered and the ...
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Yueqiu Zhang, Shiliang Liu, Fangyan Cheng and Zhenyao Shen
China is the largest country in terms of population and its booming urbanization has exerted negative effects on ground-surface hydrological processes at different spatial scales, land-use types, and water balance, such as surface runoff, groundwater rec...
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Dibesh Khadka, Mukand S. Babel and Ambili G. Kamalamma
Climate change (CC) and land-use change (LUC) will alter a basin?s hydrological processes and water balance. Quantifying their significance is imperative in formulating appropriate countermeasures and management plans. This study assesses projected chang...
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Rosa Mediavilla, Juan I. Santisteban, Ignacio López-Cilla, Luis Galán de Frutos and África de la Hera-Portillo
Wetlands are environments whose water balance is highly sensitive to climate change and human action. This sensitivity has allowed us to explore the relationships between surface water and groundwater in the long term as their sediments record all these ...
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Ali Nadir Arslan and Zuhal Akyürek
Snow cover is an essential climate variable directly affecting the Earth?s energy balance. Snow cover has a number of important physical properties that exert an influence on global and regional energy, water, and carbon cycles. Remote sensing provides a...
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Yong Tian, Jianzhi Xiong, Xin He, Xuehui Pi, Shijie Jiang, Feng Han and Yi Zheng
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 eva...
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Miguel Rodríguez-Rodríguez, Ana Fernández-Ayuso, Masaki Hayashi and Francisco Moral-Martos
The physical limnology of a shallow pond system was characterized using field measurements of water temperature, pH, and electrical conductivity (EC). We determined the spatial variability in surface and groundwater temperature, pH, and EC along the pond...
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Hok Sum Fok, Linghao Zhou and Hang Ji
A suitable routing model for predicting future monthly water discharge (WD) is essential for operational hydrology, including water supply, and hydrological extreme management, to mention but a few. This is particularly important for a remote area withou...
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Ryan T. Bailey, Katrin Bieger, Jeffrey G. Arnold and David D. Bosch
Watershed models are used worldwide to assist with water and nutrient management under conditions of changing climate, land use, and population. Of these models, the Soil and Water Assessment Tool (SWAT) and SWAT+ are the most widely used, although their...
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Ali Salem, József Dezso and Mustafa El-Rawy
The assessment of spatial and temporal distribution of groundwater recharge is required as an input to develop the regional groundwater model in the Drava flood plain for more accurate simulations of different management scenarios. WetSpass-M, a GIS-base...
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Camila Andrade Abe, Felipe De Lucia Lobo, Yonas Berhan Dibike, Maycira Pereira de Farias Costa, Vanessa Dos Santos and Evlyn Márcia L. M. Novo
Land cover changes (LCC) affect the water balance (WB), changing surface runoff (SurfQ), evapotranspiration (ET), groundwater (GW) regimes, and streamflow (Q). The Tapajós Basin (southeastern Amazon) has experienced LCC over the last 40 years, with incre...
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Vanessa de Arruda Souza, Débora Regina Roberti, Anderson Luis Ruhoff, Tamíres Zimmer, Daniela Santini Adamatti, Luis Gustavo G. de Gonçalves, Marcelo Bortoluzzi Diaz, Rita de Cássia Marques Alves and Osvaldo L. L. de Moraes
Evapotranspiration (ET) is an important component of the hydrological cycle. Understanding the ET process has become of fundamental importance given the scenario of global change and increasing water use, especially in the agricultural sector. Determinin...
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Franklin Paredes-Trejo, Barlin O. Olivares, Yair Movil-Fuentes, Juan Arevalo-Groening and Alfredo Gil
Droughts impact the water cycle, ecological balance, and socio-economic development in various regions around the world. The Orinoco River Basin is a region highly susceptible to droughts. The basin supports diverse ecosystems and supplies valuable resou...
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George Bariamis and Evangelos Baltas
Identifying the core hydrological processes of catchments is a critical step for operative hydrological modeling. This study attempts to assess the long-term alterations in streamflow in three adjacent catchments of Upper East Fork White River, Indiana U...
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Frauke Kachholz and Jens Tränckner
Land use changes influence the water balance and often increase surface runoff. The resulting impacts on river flow, water level, and flood should be identified beforehand in the phase of spatial planning. In two consecutive papers, we develop a model-ba...
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Johan van Tol, George van Zijl and Stefan Julich
Soil information is critical in watershed-scale hydrological modelling; however, it is still debated which level of complexity the soil data should contain. In the present study, we have compared the effect of two levels of soil data on the hydrologic si...
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Minh Tuan Bui, Jinmei Lu and Linmei Nie
The Arctic region is the most sensitive region to climate change. Hydrological models are fundamental tools for climate change impact assessment. However, due to the extreme weather conditions, specific hydrological process, and data acquisition challeng...
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Haochun Du, Hok Sum Fok, Yutong Chen and Zhongtian Ma
Storage and runoff are the two fundamental surface hydrological variables of a catchment. Research studies have been focused on the storage-runoff (S-R) hysteretic relationship of a catchment and its explanation very recently, thanks to satellite gravime...
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Girma Y Ebrahim, Jonathan F. Lautze and Karen G. Villholth
Climatic variability and change result in unreliable and uncertain water availability and contribute to water insecurity in Africa, particularly in arid and semi-arid areas and where water storage infrastructure is limited. Managed aquifer recharge (MAR)...
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Tonantzin Tarin,Enrico A. Yepez,Jaime Garatuza-Payan,Julio C. Rodriguez,Luis A. Méndez-Barroso,Christopher J. Watts,Enrique R. Vivoni
Pág. 319 - 335
Evapotranspiration is the second largest component of the hydrological cycle after rainfall precipitation in semiarid regions such as northwestern Mexico. In this study, we partitioned the evapotranspiration (ET) flux using stable isotopes of water in th...
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