Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope Measurements

Abstract Variations in tree water sources are important to understand in semi‐arid ecosystems because climatic shifts towards lower snowpack and increased drought affect water availability in subalpine forests of the western US. Here, we use daily in situ measurements of stable isotopes (2H & 18...

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Main Authors: Matthias Sprenger, Stefan Seeger, Max Berkelhammer, Nathaniel A. Bogie, Raymond J. Hess, Wendy S. Brown, Sylvain Kuppel, James Knighton
Format: Article
Language:English
Published: Wiley 2025-08-01
Series:Water Resources Research
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Online Access:https://doi.org/10.1029/2024WR039171
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author Matthias Sprenger
Stefan Seeger
Max Berkelhammer
Nathaniel A. Bogie
Raymond J. Hess
Wendy S. Brown
Sylvain Kuppel
James Knighton
author_facet Matthias Sprenger
Stefan Seeger
Max Berkelhammer
Nathaniel A. Bogie
Raymond J. Hess
Wendy S. Brown
Sylvain Kuppel
James Knighton
author_sort Matthias Sprenger
collection DOAJ
description Abstract Variations in tree water sources are important to understand in semi‐arid ecosystems because climatic shifts towards lower snowpack and increased drought affect water availability in subalpine forests of the western US. Here, we use daily in situ measurements of stable isotopes (2H & 18O) in soil and tree stem water, soil matric potential and sap flow to study tree water uptake dynamics. We instrumented three soil profiles down to 90 cm, as well as three aspen and engelmann spruce trees near Gothic, Colorado, in the East River watershed. We observed the fate of natural isotopic variations in rainfall, soil, and plants from June to October 2022, and in August 2023 we conducted a 2H labeled irrigation experiment. Our observations showed that all studied aspen trees compensated for water scarcity in the shallow soil by shifting the dominant water source at 60(±20) cm to ⅔ of uptake from 90 cm within a few days of a dry period. Both species relied on snowmelt stored in the subsoil to sustain transpiration. Intense rainfall caused the plant water uptake to shift partially to top soil layers within 2 days. Spruce transpiration was lower and relied more on snowmelt, because rainfall infiltration was low in the spruce stand due to high canopy interception. Our findings highlight the important role of snowmelt stored in the deep soil layers for subalpine forest drought response and the dominant fate of monsoonal rainfall to become transpiration rather than recharging groundwater and streams in the Upper Colorado River.
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spelling doaj-art-27b5c407bb0f43d7a1b8be2ed82271d22025-08-26T12:02:54ZengWileyWater Resources Research0043-13971944-79732025-08-01618n/an/a10.1029/2024WR039171Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope MeasurementsMatthias Sprenger0Stefan Seeger1Max Berkelhammer2Nathaniel A. Bogie3Raymond J. Hess4Wendy S. Brown5Sylvain Kuppel6James Knighton7Lawrence Berkeley National Laboratory Berkeley CA USADepartment of Crop Sciences Chair of Soil Physics University of Göttingen Göttingen GermanyDepartment of Earth and Environmental Sciences University of Illinois Chicago Chicago IL USADepartment of Geology San José State University San Jose CA USADepartment of Earth and Environmental Sciences Rutgers University Newark NJ USAThe Rocky Mountain Biological Laboratory Crested Butte CO USAGéosciences Environment Toulouse CNRS ‐ IRD ‐ UT3 ‐ CNES Toulouse FranceDepartment of Natural Resources and the Environment University of Connecticut Storrs CT USAAbstract Variations in tree water sources are important to understand in semi‐arid ecosystems because climatic shifts towards lower snowpack and increased drought affect water availability in subalpine forests of the western US. Here, we use daily in situ measurements of stable isotopes (2H & 18O) in soil and tree stem water, soil matric potential and sap flow to study tree water uptake dynamics. We instrumented three soil profiles down to 90 cm, as well as three aspen and engelmann spruce trees near Gothic, Colorado, in the East River watershed. We observed the fate of natural isotopic variations in rainfall, soil, and plants from June to October 2022, and in August 2023 we conducted a 2H labeled irrigation experiment. Our observations showed that all studied aspen trees compensated for water scarcity in the shallow soil by shifting the dominant water source at 60(±20) cm to ⅔ of uptake from 90 cm within a few days of a dry period. Both species relied on snowmelt stored in the subsoil to sustain transpiration. Intense rainfall caused the plant water uptake to shift partially to top soil layers within 2 days. Spruce transpiration was lower and relied more on snowmelt, because rainfall infiltration was low in the spruce stand due to high canopy interception. Our findings highlight the important role of snowmelt stored in the deep soil layers for subalpine forest drought response and the dominant fate of monsoonal rainfall to become transpiration rather than recharging groundwater and streams in the Upper Colorado River.https://doi.org/10.1029/2024WR039171stable isotopesEcohydrologyisotope hydrologyplant water uptakevadose zonecritical zone
spellingShingle Matthias Sprenger
Stefan Seeger
Max Berkelhammer
Nathaniel A. Bogie
Raymond J. Hess
Wendy S. Brown
Sylvain Kuppel
James Knighton
Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope Measurements
Water Resources Research
stable isotopes
Ecohydrology
isotope hydrology
plant water uptake
vadose zone
critical zone
title Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope Measurements
title_full Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope Measurements
title_fullStr Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope Measurements
title_full_unstemmed Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope Measurements
title_short Opportunistic Short‐Term Water Uptake Dynamics by Subalpine Trees Observed via In Situ Water Isotope Measurements
title_sort opportunistic short term water uptake dynamics by subalpine trees observed via in situ water isotope measurements
topic stable isotopes
Ecohydrology
isotope hydrology
plant water uptake
vadose zone
critical zone
url https://doi.org/10.1029/2024WR039171
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