2013
DOI: 10.1111/jawr.12130
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Modeling the Fate and Transport of Plunging Inflows to Onondaga Lake

Abstract: The transport and fate of two plunging tributaries, Onondaga and Ninemile Creeks, in Onondaga Lake, New York, are quantified based on application of hydrodynamic/transport models. Short-term transport is simulated with a three-dimensional Estuary Lake and Coastal Ocean Model (ELCOM), while the longer term fate is represented by a previously validated one-dimensional model (UFILS4). The validation of ELCOM for the vertical distribution of tributary inflow into the lake's water column is demonstrated for four dy… Show more

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Cited by 8 publications
(20 citation statements)
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“…Bacteria mediated losses are likely operative, though not presently quantified. Secondly, the contemporary tributary contributions to the summertime TDP L to the upper waters (Figure 2) are overestimated because these do not accommodate the effects of plunging that prevails to varying extents for important tributaries [35][36][37].…”
Section: Water Quality Benefits Of a Deep Offshore Dischargementioning
confidence: 99%
“…Bacteria mediated losses are likely operative, though not presently quantified. Secondly, the contemporary tributary contributions to the summertime TDP L to the upper waters (Figure 2) are overestimated because these do not accommodate the effects of plunging that prevails to varying extents for important tributaries [35][36][37].…”
Section: Water Quality Benefits Of a Deep Offshore Dischargementioning
confidence: 99%
“…Matthews et al ., , unpublished data), respectively, was consistent with the differences in negative buoyancy of these inputs (Figure ). These efficiencies are subject to substantial short‐term variations in response to the dynamics of ambient mixing and runoff (Owens et al ., ). Moreover, the same ordering for the entry depth from plunging was predicted (e.g., Metro the shallowest).…”
Section: Resultsmentioning
confidence: 97%
“…The plunging of the tributaries and Metro diminishes the impacts of the external loads delivered by these inflows relative to upper mixed layer entries for issues of the upper lake waters, such as primary production (trophic state) (Effler et al ., , ) and acceptable FC levels for contact recreation (Canale et al ., ). The plunging phenomenon likely occurs more widely than is presently recognized (Owens et al ., ). Where the phenomenon is not recognized, the expected or model projected benefits for a lake from systematic loading reductions in negatively buoyant inflows will be overstated.…”
Section: Resultsmentioning
confidence: 99%
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