Hydrological connectivity in intermittent rivers and ephemeral streams

Andrew Boulton, Robert ROLLS, Kris Jaeger, Thibault Datry

    Research output: A Conference proceeding or a Chapter in BookChapter

    6 Citations (Scopus)

    Abstract

    In intermittent rivers and ephemeral streams (hereafter, IRES), hydrological connectivity mediated by either flowing or nonflowing water extends along three spatial dimensions-longitudinal, lateral, and vertical-and varies over time. Flow intermittence disrupts this connectivity, operating through complex hydrological transitions (e.g., between flowing and nonflowing phases). These transitions occur concurrently and interact along all three spatial dimensions, primarily driven by flow regime and catchment geomorphology, modified by human activities. Longitudinally, streamflow cessation and drying interrupt hydrological connectivity, contributing to physicochemical patchiness, habitat isolation, and fragmentation of metapopulations and metacommunities. Laterally, hydrological connectivity established during overbank flows is lost when water levels fall, reducing water-mediated transfers of energy, materials, and organisms from the floodplain and riparian zone. Vertically, flow cessation impairs exchange of surface and shallow groundwater, severely altering hydrological, chemical, and microbial gradients within the sediments. Concurrent interactions and physical discontinuities in hydrological connectivity along these three dimensions produce complex mosaics of physicochemical patches at different scales whose boundaries fluctuate over time in response to the flow regime. This complex patchiness underpins the characteristic physical, chemical, and biological diversity at multiple scales along longitudinal, lateral, and vertical hydrological dimensions in IRES.

    Original languageEnglish
    Title of host publicationIntermittent Rivers and Ephemeral Streams
    Subtitle of host publicationEcology and Management
    EditorsThibault Datry, Nuria Bonada, Andrew Boulton
    Place of PublicationLondon
    PublisherElsevier
    Pages79-108
    Number of pages30
    ISBN (Electronic)9780128039045
    ISBN (Print)9780128038352
    DOIs
    Publication statusPublished - 2017

    Fingerprint

    ephemeral stream
    connectivity
    river
    patchiness
    overbank flow
    riparian zone
    metapopulation
    geomorphology
    streamflow
    floodplain
    discontinuity
    fragmentation
    water level
    human activity
    catchment
    water
    groundwater
    habitat
    sediment
    energy

    Cite this

    Boulton, A., ROLLS, R., Jaeger, K., & Datry, T. (2017). Hydrological connectivity in intermittent rivers and ephemeral streams. In T. Datry, N. Bonada, & A. Boulton (Eds.), Intermittent Rivers and Ephemeral Streams: Ecology and Management (pp. 79-108). London: Elsevier. https://doi.org/10.1016/B978-0-12-803835-2.00004-8
    Boulton, Andrew ; ROLLS, Robert ; Jaeger, Kris ; Datry, Thibault. / Hydrological connectivity in intermittent rivers and ephemeral streams. Intermittent Rivers and Ephemeral Streams: Ecology and Management. editor / Thibault Datry ; Nuria Bonada ; Andrew Boulton. London : Elsevier, 2017. pp. 79-108
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    abstract = "In intermittent rivers and ephemeral streams (hereafter, IRES), hydrological connectivity mediated by either flowing or nonflowing water extends along three spatial dimensions-longitudinal, lateral, and vertical-and varies over time. Flow intermittence disrupts this connectivity, operating through complex hydrological transitions (e.g., between flowing and nonflowing phases). These transitions occur concurrently and interact along all three spatial dimensions, primarily driven by flow regime and catchment geomorphology, modified by human activities. Longitudinally, streamflow cessation and drying interrupt hydrological connectivity, contributing to physicochemical patchiness, habitat isolation, and fragmentation of metapopulations and metacommunities. Laterally, hydrological connectivity established during overbank flows is lost when water levels fall, reducing water-mediated transfers of energy, materials, and organisms from the floodplain and riparian zone. Vertically, flow cessation impairs exchange of surface and shallow groundwater, severely altering hydrological, chemical, and microbial gradients within the sediments. Concurrent interactions and physical discontinuities in hydrological connectivity along these three dimensions produce complex mosaics of physicochemical patches at different scales whose boundaries fluctuate over time in response to the flow regime. This complex patchiness underpins the characteristic physical, chemical, and biological diversity at multiple scales along longitudinal, lateral, and vertical hydrological dimensions in IRES.",
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    author = "Andrew Boulton and Robert ROLLS and Kris Jaeger and Thibault Datry",
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    Boulton, A, ROLLS, R, Jaeger, K & Datry, T 2017, Hydrological connectivity in intermittent rivers and ephemeral streams. in T Datry, N Bonada & A Boulton (eds), Intermittent Rivers and Ephemeral Streams: Ecology and Management. Elsevier, London, pp. 79-108. https://doi.org/10.1016/B978-0-12-803835-2.00004-8

    Hydrological connectivity in intermittent rivers and ephemeral streams. / Boulton, Andrew ; ROLLS, Robert; Jaeger, Kris ; Datry, Thibault.

    Intermittent Rivers and Ephemeral Streams: Ecology and Management. ed. / Thibault Datry; Nuria Bonada; Andrew Boulton. London : Elsevier, 2017. p. 79-108.

    Research output: A Conference proceeding or a Chapter in BookChapter

    TY - CHAP

    T1 - Hydrological connectivity in intermittent rivers and ephemeral streams

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    AU - ROLLS, Robert

    AU - Jaeger, Kris

    AU - Datry, Thibault

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    N2 - In intermittent rivers and ephemeral streams (hereafter, IRES), hydrological connectivity mediated by either flowing or nonflowing water extends along three spatial dimensions-longitudinal, lateral, and vertical-and varies over time. Flow intermittence disrupts this connectivity, operating through complex hydrological transitions (e.g., between flowing and nonflowing phases). These transitions occur concurrently and interact along all three spatial dimensions, primarily driven by flow regime and catchment geomorphology, modified by human activities. Longitudinally, streamflow cessation and drying interrupt hydrological connectivity, contributing to physicochemical patchiness, habitat isolation, and fragmentation of metapopulations and metacommunities. Laterally, hydrological connectivity established during overbank flows is lost when water levels fall, reducing water-mediated transfers of energy, materials, and organisms from the floodplain and riparian zone. Vertically, flow cessation impairs exchange of surface and shallow groundwater, severely altering hydrological, chemical, and microbial gradients within the sediments. Concurrent interactions and physical discontinuities in hydrological connectivity along these three dimensions produce complex mosaics of physicochemical patches at different scales whose boundaries fluctuate over time in response to the flow regime. This complex patchiness underpins the characteristic physical, chemical, and biological diversity at multiple scales along longitudinal, lateral, and vertical hydrological dimensions in IRES.

    AB - In intermittent rivers and ephemeral streams (hereafter, IRES), hydrological connectivity mediated by either flowing or nonflowing water extends along three spatial dimensions-longitudinal, lateral, and vertical-and varies over time. Flow intermittence disrupts this connectivity, operating through complex hydrological transitions (e.g., between flowing and nonflowing phases). These transitions occur concurrently and interact along all three spatial dimensions, primarily driven by flow regime and catchment geomorphology, modified by human activities. Longitudinally, streamflow cessation and drying interrupt hydrological connectivity, contributing to physicochemical patchiness, habitat isolation, and fragmentation of metapopulations and metacommunities. Laterally, hydrological connectivity established during overbank flows is lost when water levels fall, reducing water-mediated transfers of energy, materials, and organisms from the floodplain and riparian zone. Vertically, flow cessation impairs exchange of surface and shallow groundwater, severely altering hydrological, chemical, and microbial gradients within the sediments. Concurrent interactions and physical discontinuities in hydrological connectivity along these three dimensions produce complex mosaics of physicochemical patches at different scales whose boundaries fluctuate over time in response to the flow regime. This complex patchiness underpins the characteristic physical, chemical, and biological diversity at multiple scales along longitudinal, lateral, and vertical hydrological dimensions in IRES.

    KW - Drying

    KW - Environmental management

    KW - Floodplains

    KW - Flow regime

    KW - Fluvial geomorphology

    KW - Habitat fragmentation

    KW - Hydrological connectivity

    KW - Hydrology

    KW - Hyporheic zone

    KW - Intermittence

    KW - Water regime

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    UR - http://www.mendeley.com/research/hydrological-connectivity-intermittent-rivers-ephemeral-streams

    U2 - 10.1016/B978-0-12-803835-2.00004-8

    DO - 10.1016/B978-0-12-803835-2.00004-8

    M3 - Chapter

    SN - 9780128038352

    SP - 79

    EP - 108

    BT - Intermittent Rivers and Ephemeral Streams

    A2 - Datry, Thibault

    A2 - Bonada, Nuria

    A2 - Boulton, Andrew

    PB - Elsevier

    CY - London

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    Boulton A, ROLLS R, Jaeger K, Datry T. Hydrological connectivity in intermittent rivers and ephemeral streams. In Datry T, Bonada N, Boulton A, editors, Intermittent Rivers and Ephemeral Streams: Ecology and Management. London: Elsevier. 2017. p. 79-108 https://doi.org/10.1016/B978-0-12-803835-2.00004-8