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  • Mathew, Rooni  (3)
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  • 1
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2017
    In:  Ocean Dynamics Vol. 67, No. 6 ( 2017-6), p. 691-712
    In: Ocean Dynamics, Springer Science and Business Media LLC, Vol. 67, No. 6 ( 2017-6), p. 691-712
    Type of Medium: Online Resource
    ISSN: 1616-7341 , 1616-7228
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2017
    detail.hit.zdb_id: 2063267-8
    detail.hit.zdb_id: 201122-0
    SSG: 14
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    Elsevier BV ; 2022
    In:  Advances in Water Resources Vol. 166 ( 2022-08), p. 104224-
    In: Advances in Water Resources, Elsevier BV, Vol. 166 ( 2022-08), p. 104224-
    Type of Medium: Online Resource
    ISSN: 0309-1708
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2022
    detail.hit.zdb_id: 2023320-6
    detail.hit.zdb_id: 428761-7
    SSG: 14
    Location Call Number Limitation Availability
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  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2020
    In:  Ocean Dynamics Vol. 70, No. 4 ( 2020-04), p. 435-462
    In: Ocean Dynamics, Springer Science and Business Media LLC, Vol. 70, No. 4 ( 2020-04), p. 435-462
    Abstract: Estuarine sediment dynamics are a consequence of various forcings (barotropic, estuarine circulation, and fluvial) that vary in space and time. Here, we present a study examining sediment dynamics in a narrow microtidal estuary, the Lower Passaic River in New Jersey, USA. The analysis incorporates measurements of suspended sediments, morphological change, sediment erodibility, and a numerical hydrodynamic model. The former two datasets are used to develop an understanding of sediment dynamics over the full range of hydrologic conditions, and the latter two datasets are used to interpret the behavior of the system. Subsequently, a conceptual picture is developed, one that classifies the morphological status of the system at any given time into three regimes dependent on river flow—regime I includes conditions when the system is importing sediments, regime II includes conditions when the system is exporting sediments by flushing a thin easily erodible surficial stratum termed the fluff layer, and regime III includes conditions when the system is exporting sediments by scouring more consolidated strata underneath the fluff layer. Regime III is relevant for the long-term morphodynamic equilibrium of the estuary by providing a mechanism that erodes and exports sediment accumulated under regime I conditions. Consequently, sediment dynamics depend not only on short time-scale processes such as the instantaneous river flow rate, but also on the time-history of river flow, and the long-term morphological progression of the system. These regimes represent a conceptualization of estuarine sediment transport dynamics and can be useful in the development of effective estuarine sediment management strategies.
    Type of Medium: Online Resource
    ISSN: 1616-7341 , 1616-7228
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2020
    detail.hit.zdb_id: 2063267-8
    detail.hit.zdb_id: 201122-0
    SSG: 14
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
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