2000
DOI: 10.1007/978-94-015-9472-1_4
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Definition, Effects and Assessment of Groundwater Droughts

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Cited by 87 publications
(65 citation statements)
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“…This is followed by the critical threshold of cease-toflow after which streams become a series of pools that in severe drought may themselves disappear (Boulton, 2003;Lake, 2003). As drought depletes surface waters, it should be noted that groundwater levels and volumes may, with time, start to be reduced (Van Lanen & Peters, 2000). Groundwater drought is poorly understood, but it is critical to recognise that groundwater often forms the base flow of surface systems and also that many wetland systems are groundwater-dependent.…”
Section: What Is Drought?mentioning
confidence: 99%
“…This is followed by the critical threshold of cease-toflow after which streams become a series of pools that in severe drought may themselves disappear (Boulton, 2003;Lake, 2003). As drought depletes surface waters, it should be noted that groundwater levels and volumes may, with time, start to be reduced (Van Lanen & Peters, 2000). Groundwater drought is poorly understood, but it is critical to recognise that groundwater often forms the base flow of surface systems and also that many wetland systems are groundwater-dependent.…”
Section: What Is Drought?mentioning
confidence: 99%
“…Under natural conditions, groundwater drought is caused by a lack of precipitation followed by a decrease in recharge, resulting in decreases in GWL and discharge and eventually a decline in the available groundwater [49]. The "lack of precipitation" is usually determined by a comparison with a "normal" condition or a mean value from past measurements [49].…”
Section: Threshold Level Methodsmentioning
confidence: 99%
“…The "lack of precipitation" is usually determined by a comparison with a "normal" condition or a mean value from past measurements [49]. As noted by Mishra and Singh [31], the reason for analyzing the change in GWL rather than groundwater storage is that "defining or estimating the total available water is difficult and in most groundwater systems, negative impacts of storage depletion can be felt, long before the total volume of groundwater in storage is decreased" [49,50]. Therefore, most groundwater droughts are defined as water-level declines [28,29].…”
Section: Threshold Level Methodsmentioning
confidence: 99%
“…Groundwater drought, which is a type of hydrological drought characterized by sustained low groundwater levels, reduced baseflow, and reduced flows to springs and groundwater-fed rivers and wetlands [3,4], has profound adverse impacts on water resources such as groundwater discharge to the groundwater-dependent surface waters and ecosystems, and also affects public water supply, industry supplies, and agricultural irrigation [5].…”
Section: Introductionmentioning
confidence: 99%