Effects of climate change on depression‐focused groundwater recharge in the Canadian Prairies [PDF]
Vadose Zone Journal, 2021 Small topographic depressions are ubiquitous in the glaciated terrain of the Northern Prairies characterized by a cold semiarid climate. Groundwater recharge in this region is focused in topographic depressions, which receive lateral inputs of snowmelt ...
Amro Negm +3 more
doaj +4 more sources
A Coupled Soil Water Balance Model for Simulating Depression-Focused Groundwater Recharge [PDF]
Vadose Zone Journal, 2018 In arid and semiarid environments, focused infiltration of rain and snowmelt water under topographic depressions is an important mechanism of groundwater recharge.
Saskia L. Noorduijn +3 more
doaj +3 more sources
Ephemeral Ponds: Are They the Dominant Source of Depression‐Focused Groundwater Recharge? [PDF]
Water Resources Research, 2020 AbstractDepression‐focused recharge is a concept proposed to explain groundwater recharge in the prairie regions of North America. Topographic depressions in this hummocky landscape collect blowing snow and snowmelt, and occasional runoff during rainfall events.
Garth van der Kamp +4 more
openaire +3 more sources
Quantifying seasonal, depression focused recharge in the context of public supply well vulnerability [PDF]
Hydrological Processes, 2023 AbstractDepression focused recharge (DFR) may be a hydrologically important process that impacts the vulnerability of public supply wells, specifically related to pathogenic contaminants. The nature of DFR in glacial moraine environments, such as those located in northern latitudes within North America and Europe, is less well established than in other
Andrew J. Wiebe +2 more
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Integrated hydrogeological and geophysical study of depression‐focused groundwater recharge in the Canadian prairies [PDF]
Water Resources Research, 2004 In the northern prairie region of North America, numerous seasonal wetlands and ephemeral ponds form as snowmelt water is trapped in small topographical depressions. A detailed hydrogeological investigation is combined with electrical resistivity imaging (ERI) to evaluate the roles of the wetlands and ponds on depression‐focused groundwater recharge at
Masaki Hayashi +2 more
openaire +3 more sources
Journal of Groundwater Science and Engineering, 2023 The North China Plain is one of the main grain producing areas in China. However, over-exploitation has long been unsustainable since the water supply is mainly from groundwater.
Rui-fang Meng +6 more
doaj +1 more source
Sensors, 2021 In semi-arid ecoregions of temperate zones, focused snowmelt water infiltration in topographic depressions is a key, but imperfectly understood, groundwater recharge mechanism. Routine monitoring is precluded by the abundance of depressions. We have used
Pavel P Fil +3 more
doaj +1 more source
Effects of preferential flow on snowmelt partitioning and groundwater recharge in frozen soils [PDF]
Hydrology and Earth System Sciences, 2019 Snowmelt is a major source of groundwater recharge in cold regions. Throughout many landscapes snowmelt occurs when the ground is still frozen; thus frozen soil processes play an important role in snowmelt routing, and, by extension, the timing and ...
A. A. Mohammed +4 more
doaj +1 more source
Estimation of temporal and spatial variations in groundwater recharge in unconfined sand aquifers using Scots pine inventories [PDF]
, 2014 Acknowledgements. This study was made possible through funding from the EU 7th Framework programme GENESIS (contract number 226536), AQVI project (no. 128377) in Academy of Finland AKVA research programme, the Renlund Foundation, VALUE doctoral school ...
Ala-Aho, P., Kløve, B., Rossi, P. M.
core +2 more sources
Storm-water infiltration and focused recharge modeling with finite-volume two-dimensional Richards equation: application to an experimental rain garden [PDF]
, 2009 Rain gardens are infiltration systems that provide volume and water quality control, recharge enhancement, as well as landscape, ecological, and economic benefits.
Alejandro Dussaillant +6 more
core +1 more source