Cited by 32Hydrology and Watershed Management StudiesFish Ecology and Management StudiesWater Quality and Resources Studies

Residence‐time‐based classification of surface water systems

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Jones, Allan E., Hodges, Ben R., McClelland, James W., Hardison, Amber K., Moffett, Kevan B.·2017·Water Resources Research

Abstract

Defining surface water systems as lentic or lotic is an important first step in linking hydrology and ecology. Existing approaches for classifying surface water as lentic (reservoir‐like) or lotic (river‐like) use qualitative observations, solitary snapshot measurements in time and space, or ecologic metrics that are not broadly repeatable. This study introduces the Freshwater Continuum Classification (FCC), a quantitative method to consistently and objectively classify lentic/lotic systems based on integrated residence time (iT R), the time incoming water would take to exit the system given observed temporal variations in the system's discharge and volume. Lentic/lotic classification is determined from comparison of median iT R with critical flow thresholds related to key time scales such as zooplankton generation. Some systems switch between lentic and lotic behaviors over time, which are additionally defined in the FCC as oscillic. Pilot application of the FCC to 15 tidally influenced river segments along the Texas Gulf Coast produced good agreement with previous methods of determining lentic/lotic character. The FCC defined 8 of 15 tidal reaches as primarily lentic, 6 as intermediate, and 1 as lotic between October 2007 and March 2015. Of the 15 reaches, 9 were also oscillic, characterized in this climate by short‐lived lotic character during flash floods. The FCC provides a broadly applicable, repeatable, quantitative method to classify surface water bodies as lentic/intermediate/lotic and oscillic/nonoscillic regardless of size or nature (e.g., river or reservoir) based on system volume and flow characteristics.

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  • The degree of biogeochemical processing in ditches is controlled mainly by residence time, as observed in other inland waters.

    “The degree of biogeochemical processing is controlled mainly by residence time (the amount of time water spends in the ditch before flowing elsewhere), as observed in other inland waters 126,127 .”

    From Lines in the landscape (2025) · cites this paper as [127]

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Research works printed but not linked: 2

  1. Evans, A., K. Madden, and S. M. Palmer (Eds.) (2012), The Ecology and Sociology of the Mission-Aransas Estuary, Mission-Aransas Natl. Estua- rine Res. Reserve, 200 pp., Port Aransas, Tex.
  2. Intergovernmental Panel on Climate Change (IPCC) (2013), Climate change 2013: The physical science basis, in Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by T. F. Stocker, 1535 pp., Cambridge Univ. Press, Cambridge, U. K.

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Authors
Jones, A. E., Hodges, B. R., McClelland, J. W., Hardison, A. K., & Moffett, K. B.
Affiliations
  • The University of Texas at Austin (US)
  • University of Texas at Austin Marine Science Institute (US)
  • Washington State University Vancouver (US)
Corresponding author
Jones, Allan E.
Venue
Water Resources Research
Published
2017-07
Volume
53
Issue
7
Pages
5567-5584
ISSN
  • 0043-1397 (ISSN-L)
  • 1944-7973
OpenAlex
W2717727395
Cited by
32
References
41
Citations by year
2026: 4 · 2025: 4 · 2024: 4 · 2023: 4 · 2022: 6 · 2021: 3 · 2020: 4 · 2019: 2 · 2018: 1
FWCI
1.02
Type
journal article
Language
en
Open access
Locations
Water Resources Research (publishedVersion)
Funders
National Science Foundation (1417433, 1331610)
Topics
  • Physical Sciences › Environmental Science › Water Science and Technology › Hydrology and Watershed Management Studies
  • Physical Sciences › Environmental Science › Nature and Landscape Conservation › Fish Ecology and Management Studies
  • Physical Sciences › Environmental Science › Water Science and Technology › Water Quality and Resources Studies
Keywords
residence time, surface water systems, tidal rivers, flash floods, Texas coast

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