2002
DOI: 10.1006/qres.2002.2377
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Mid-Holocene Hydrologic Model of the Shingobee Watershed, Minnesota

Abstract: A hydrologic model of the Shingobee Watershed in north-central Minnesota was developed to reconstruct mid-Holocene paleo-lake levels for Williams Lake, a surface-water body located in the southern portion of the watershed. Hydrologic parameters for the model were first estimated in a calibration exercise using a 9-yr historical record (1990)(1991)(1992)(1993)(1994)(1995)(1996)(1997)(1998) of climatic and hydrologic stresses. The model reproduced observed temporal and spatial trends in surface/groundwater level… Show more

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Cited by 26 publications
(26 citation statements)
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“…The hydraulic properties of the outwash sands have been measured by over 20 aquifer tests. Hydraulic conductivity values measured by single and multi-well aquifer tests performed at the northern edge of the watershed within the outwash sands ranged from 9.15!10 K7 to 1.72!10 K3 m s K1 (Filby et al, 2002).…”
Section: Study Areamentioning
confidence: 99%
“…The hydraulic properties of the outwash sands have been measured by over 20 aquifer tests. Hydraulic conductivity values measured by single and multi-well aquifer tests performed at the northern edge of the watershed within the outwash sands ranged from 9.15!10 K7 to 1.72!10 K3 m s K1 (Filby et al, 2002).…”
Section: Study Areamentioning
confidence: 99%
“…This study, along with those by Almendinger (1993), Filby et al (2002), Smith et al (2002), and Donovan et al (2002), demonstrates that interpretations of the effect of climatic change on lake levels need to consider groundwater hydrodynamics and analysis of the relative positions of the lakes within watersheds as well as local permeability. Lakes hosted in relatively low-permeability tills in our model underwent larger lake-stage changes during the mid-Holocene than did those lakes situated in relatively sandy deposits.…”
Section: Discussionmentioning
confidence: 68%
“…on February 4, 2016 gsabulletin.gsapubs.org Downloaded from Filby et al, 2002), and dune activity (Forman et al, 2001). Locke (1995) used pollen-transfer functions of Whitlock et al (1993) and pollen data from Williams Lake sediment cores from the Shingobee Watershed (Fig.…”
Section: Minnesota's Holocene Climatic Historymentioning
confidence: 99%
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