Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic Exchange

Abstract Field studies of hyporheic exchange in mountain systems are often conducted using short study reaches and a limited number of observations. It is common practice to assume these study reaches represent hyporheic exchange at larger scales or different sites and to infer general relationships...

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Main Authors: Paige S. Becker, Adam S. Ward, Skuyler P. Herzog, Steven M. Wondzell
Format: Article
Language:English
Published: Wiley 2023-01-01
Series:Water Resources Research
Online Access:https://doi.org/10.1029/2022WR032718
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author Paige S. Becker
Adam S. Ward
Skuyler P. Herzog
Steven M. Wondzell
author_facet Paige S. Becker
Adam S. Ward
Skuyler P. Herzog
Steven M. Wondzell
author_sort Paige S. Becker
collection DOAJ
description Abstract Field studies of hyporheic exchange in mountain systems are often conducted using short study reaches and a limited number of observations. It is common practice to assume these study reaches represent hyporheic exchange at larger scales or different sites and to infer general relationships among potential causal mechanisms from the limited number of observations. However, these assumptions of representativeness are rarely tested. In this study, we develop numerical models from four segments of mountain streams in different geomorphologic settings and extract shorter reaches to test how representative exchange metrics are in shorter reaches compared to their reference segments. We also map the locations of the representative reaches to determine if a pattern exists based on location. Finally, we compare variance of these shorter within‐site reaches to 29 additional reaches across the same basin to understand the impacts of inferring causal mechanisms, for example, the expectation that wide and narrow valley bottoms will yield different hyporheic exchange patterns. Our results show that the location and length strategy of the study reach must be considered before assuming an exchange metric to be representative of anything other than the exact segment studied. Further, it is necessary to quantify within and between site variations before making causal inferences based on observable characteristics, such as valley width or stream morphology. Our findings have implications for future field practices and how those practices are translated into models.
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spelling doaj-art-a8fa8e7fbe16454194d37d58decf88632025-08-20T03:27:52ZengWileyWater Resources Research0043-13971944-79732023-01-01591n/an/a10.1029/2022WR032718Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic ExchangePaige S. Becker0Adam S. Ward1Skuyler P. Herzog2Steven M. Wondzell3O’Neill School of Public and Environmental Affairs Indiana University Bloomington IN USAO’Neill School of Public and Environmental Affairs Indiana University Bloomington IN USANatural Resources Oregon State University Cascades Bend OR USAPacific Northwest Research Station U.S. Forest Service United States Department of Agriculture Corvallis OR USAAbstract Field studies of hyporheic exchange in mountain systems are often conducted using short study reaches and a limited number of observations. It is common practice to assume these study reaches represent hyporheic exchange at larger scales or different sites and to infer general relationships among potential causal mechanisms from the limited number of observations. However, these assumptions of representativeness are rarely tested. In this study, we develop numerical models from four segments of mountain streams in different geomorphologic settings and extract shorter reaches to test how representative exchange metrics are in shorter reaches compared to their reference segments. We also map the locations of the representative reaches to determine if a pattern exists based on location. Finally, we compare variance of these shorter within‐site reaches to 29 additional reaches across the same basin to understand the impacts of inferring causal mechanisms, for example, the expectation that wide and narrow valley bottoms will yield different hyporheic exchange patterns. Our results show that the location and length strategy of the study reach must be considered before assuming an exchange metric to be representative of anything other than the exact segment studied. Further, it is necessary to quantify within and between site variations before making causal inferences based on observable characteristics, such as valley width or stream morphology. Our findings have implications for future field practices and how those practices are translated into models.https://doi.org/10.1029/2022WR032718
spellingShingle Paige S. Becker
Adam S. Ward
Skuyler P. Herzog
Steven M. Wondzell
Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic Exchange
Water Resources Research
title Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic Exchange
title_full Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic Exchange
title_fullStr Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic Exchange
title_full_unstemmed Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic Exchange
title_short Testing Hidden Assumptions of Representativeness in Reach‐Scale Studies of Hyporheic Exchange
title_sort testing hidden assumptions of representativeness in reach scale studies of hyporheic exchange
url https://doi.org/10.1029/2022WR032718
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