2012
DOI: 10.3133/ofr20121140
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Simulation of groundwater flow in the shallow aquifer system of the Delmarva Peninsula, Maryland and Delaware

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Cited by 19 publications
(38 citation statements)
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“…S1), which is consistent with a water-budget-based recharge estimate for another Delmarva location of 33 cm/yr (Johnston, 1976). Sanford et al (2012) prescribed drain boundaries at root depths associated with different land uses (0.6-1.8 m below land surface), whereas we prescribed drains at the land surface in the current study. They considered the additional water removed by prescribing drains below land surface to be evapotranspiration (ET), so the recharge they applied included this ET component.…”
Section: Model Calibrationmentioning
confidence: 99%
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“…S1), which is consistent with a water-budget-based recharge estimate for another Delmarva location of 33 cm/yr (Johnston, 1976). Sanford et al (2012) prescribed drain boundaries at root depths associated with different land uses (0.6-1.8 m below land surface), whereas we prescribed drains at the land surface in the current study. They considered the additional water removed by prescribing drains below land surface to be evapotranspiration (ET), so the recharge they applied included this ET component.…”
Section: Model Calibrationmentioning
confidence: 99%
“…They considered the additional water removed by prescribing drains below land surface to be evapotranspiration (ET), so the recharge they applied included this ET component. The current study applied a net recharge value that excluded the ET component, so the reduction to 75% of the value applied by Sanford et al (2012) is reasonable. Average recharge applied to the calibrated Reference model is 43% of the 113 cm/yr mean annual precipitation recorded at the nearest NOAA rain gage (NOAA, 2010).…”
Section: Model Calibrationmentioning
confidence: 99%
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