Dependence of Aspen Stands on a Subsurface Water Subsidy: Implications for Climate Change Impacts

The reliance of 10 Utah (USA) aspen forests on direct infiltration of growing season rain versus an additional subsurface water subsidy was determined from a trait‐ and process‐based model of stomatal control. The model simulated the relationship between water supply to the root zone versus canopy t...

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Veröffentlicht in:Water resources research 2019-03, Vol.55 (3), p.1833-1848
Hauptverfasser: Love, D. M., Venturas, M. D., Sperry, J. S., Brooks, P. D., Pettit, J. L., Wang, Y., Anderegg, W. R. L., Tai, X., Mackay, D. S.
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container_end_page 1848
container_issue 3
container_start_page 1833
container_title Water resources research
container_volume 55
creator Love, D. M.
Venturas, M. D.
Sperry, J. S.
Brooks, P. D.
Pettit, J. L.
Wang, Y.
Anderegg, W. R. L.
Tai, X.
Mackay, D. S.
description The reliance of 10 Utah (USA) aspen forests on direct infiltration of growing season rain versus an additional subsurface water subsidy was determined from a trait‐ and process‐based model of stomatal control. The model simulated the relationship between water supply to the root zone versus canopy transpiration and assimilation over a growing season. Canopy flux thresholds were identified that distinguished nonstressed, stressed, and dying stands. We found growing season rain and local soil moisture were insufficient for the survival of 5 of 10 stands. Six stands required a substantial subsidy (31–80% of potential seasonal transpiration) to avoid water stress and maximize photosynthetic potential. Subsidy dependence increased with stand hydraulic conductance. Four of the six “subsidized” stands were predicted to be stressed during the survey year owing to a subsidy shortfall. Since winter snowpack is closely related to groundwater recharge in the region, we compared winter precipitation with tree‐ring chronologies. Consistent with model predictions, chronologies were more sensitive to snowpack in subsidized stands than in nonsubsidized ones. The results imply that aspen stand health in the region is more coupled to winter snowpack than to growing season water supply. Winters are predicted to have less precipitation as snow, indicating a stressful future for the region's aspen forests. Key Points Most aspen stands in Utah cannot survive on growing season rain and local soil moisture as their only water supply Aspen stands in Utah are highly dependent on a groundwater subsidy and vulnerable to any subsidy shortfall Aspen stand health in Utah will be threatened by diminished winter snowpack
doi_str_mv 10.1029/2018WR023468
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M. ; Venturas, M. D. ; Sperry, J. S. ; Brooks, P. D. ; Pettit, J. L. ; Wang, Y. ; Anderegg, W. R. L. ; Tai, X. ; Mackay, D. S.</creator><creatorcontrib>Love, D. M. ; Venturas, M. D. ; Sperry, J. S. ; Brooks, P. D. ; Pettit, J. L. ; Wang, Y. ; Anderegg, W. R. L. ; Tai, X. ; Mackay, D. S.</creatorcontrib><description>The reliance of 10 Utah (USA) aspen forests on direct infiltration of growing season rain versus an additional subsurface water subsidy was determined from a trait‐ and process‐based model of stomatal control. The model simulated the relationship between water supply to the root zone versus canopy transpiration and assimilation over a growing season. Canopy flux thresholds were identified that distinguished nonstressed, stressed, and dying stands. We found growing season rain and local soil moisture were insufficient for the survival of 5 of 10 stands. Six stands required a substantial subsidy (31–80% of potential seasonal transpiration) to avoid water stress and maximize photosynthetic potential. Subsidy dependence increased with stand hydraulic conductance. Four of the six “subsidized” stands were predicted to be stressed during the survey year owing to a subsidy shortfall. Since winter snowpack is closely related to groundwater recharge in the region, we compared winter precipitation with tree‐ring chronologies. Consistent with model predictions, chronologies were more sensitive to snowpack in subsidized stands than in nonsubsidized ones. The results imply that aspen stand health in the region is more coupled to winter snowpack than to growing season water supply. Winters are predicted to have less precipitation as snow, indicating a stressful future for the region's aspen forests. Key Points Most aspen stands in Utah cannot survive on growing season rain and local soil moisture as their only water supply Aspen stands in Utah are highly dependent on a groundwater subsidy and vulnerable to any subsidy shortfall Aspen stand health in Utah will be threatened by diminished winter snowpack</description><identifier>ISSN: 0043-1397</identifier><identifier>EISSN: 1944-7973</identifier><identifier>DOI: 10.1029/2018WR023468</identifier><language>eng</language><publisher>Washington: John Wiley &amp; Sons, Inc</publisher><subject>Atmospheric precipitations ; Canopies ; Canopy ; Climate change ; Computer simulation ; Conductance ; Dependence ; Environmental impact ; Forests ; Groundwater ; Groundwater recharge ; Growing season ; growth rings ; hydraulic conductivity ; Infiltration ; Mathematical models ; Photosynthesis ; plant hydraulics ; Precipitation ; Predictions ; Rain ; Resistance ; rhizosphere ; Root zone ; Seasons ; snow ; Snowpack ; Soil ; Soil moisture ; soil water ; Stomata ; Subsidies ; Subsurface water ; subsurface water subsidy ; Surveying ; surveys ; Survival ; Transpiration ; tree mortality ; Utah ; Water shortages ; Water stress ; Water supply ; Winter ; Winter precipitation ; xylem</subject><ispartof>Water resources research, 2019-03, Vol.55 (3), p.1833-1848</ispartof><rights>2018. American Geophysical Union. All Rights Reserved.</rights><rights>2019. American Geophysical Union. 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M.</creatorcontrib><creatorcontrib>Venturas, M. D.</creatorcontrib><creatorcontrib>Sperry, J. S.</creatorcontrib><creatorcontrib>Brooks, P. D.</creatorcontrib><creatorcontrib>Pettit, J. L.</creatorcontrib><creatorcontrib>Wang, Y.</creatorcontrib><creatorcontrib>Anderegg, W. R. L.</creatorcontrib><creatorcontrib>Tai, X.</creatorcontrib><creatorcontrib>Mackay, D. S.</creatorcontrib><title>Dependence of Aspen Stands on a Subsurface Water Subsidy: Implications for Climate Change Impacts</title><title>Water resources research</title><description>The reliance of 10 Utah (USA) aspen forests on direct infiltration of growing season rain versus an additional subsurface water subsidy was determined from a trait‐ and process‐based model of stomatal control. The model simulated the relationship between water supply to the root zone versus canopy transpiration and assimilation over a growing season. Canopy flux thresholds were identified that distinguished nonstressed, stressed, and dying stands. We found growing season rain and local soil moisture were insufficient for the survival of 5 of 10 stands. Six stands required a substantial subsidy (31–80% of potential seasonal transpiration) to avoid water stress and maximize photosynthetic potential. Subsidy dependence increased with stand hydraulic conductance. Four of the six “subsidized” stands were predicted to be stressed during the survey year owing to a subsidy shortfall. Since winter snowpack is closely related to groundwater recharge in the region, we compared winter precipitation with tree‐ring chronologies. Consistent with model predictions, chronologies were more sensitive to snowpack in subsidized stands than in nonsubsidized ones. The results imply that aspen stand health in the region is more coupled to winter snowpack than to growing season water supply. Winters are predicted to have less precipitation as snow, indicating a stressful future for the region's aspen forests. Key Points Most aspen stands in Utah cannot survive on growing season rain and local soil moisture as their only water supply Aspen stands in Utah are highly dependent on a groundwater subsidy and vulnerable to any subsidy shortfall Aspen stand health in Utah will be threatened by diminished winter snowpack</description><subject>Atmospheric precipitations</subject><subject>Canopies</subject><subject>Canopy</subject><subject>Climate change</subject><subject>Computer simulation</subject><subject>Conductance</subject><subject>Dependence</subject><subject>Environmental impact</subject><subject>Forests</subject><subject>Groundwater</subject><subject>Groundwater recharge</subject><subject>Growing season</subject><subject>growth rings</subject><subject>hydraulic conductivity</subject><subject>Infiltration</subject><subject>Mathematical models</subject><subject>Photosynthesis</subject><subject>plant hydraulics</subject><subject>Precipitation</subject><subject>Predictions</subject><subject>Rain</subject><subject>Resistance</subject><subject>rhizosphere</subject><subject>Root zone</subject><subject>Seasons</subject><subject>snow</subject><subject>Snowpack</subject><subject>Soil</subject><subject>Soil moisture</subject><subject>soil water</subject><subject>Stomata</subject><subject>Subsidies</subject><subject>Subsurface water</subject><subject>subsurface water subsidy</subject><subject>Surveying</subject><subject>surveys</subject><subject>Survival</subject><subject>Transpiration</subject><subject>tree mortality</subject><subject>Utah</subject><subject>Water shortages</subject><subject>Water stress</subject><subject>Water supply</subject><subject>Winter</subject><subject>Winter precipitation</subject><subject>xylem</subject><issn>0043-1397</issn><issn>1944-7973</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp9kD9PwzAQxS0EEqWw8QEssTAQsH2OHbNV4V-lSkgtqGPkJDakSp1iJ0L99riUATEwne7eT3fvHkLnlFxTwtQNIzRbzgkDLrIDNKKK80QqCYdoRAiHhIKSx-gkhBUhlKdCjpC-MxvjauMqgzuLJyF2eNFrVwfcOazxYijD4K2O-lL3xn8Pmnp7i6frTdtUum86F7DtPM7bZh0RnL9r92Z2uq76cIqOrG6DOfupY_T6cP-SPyWz58dpPpklGgSwhGdEZFIJpaU22oKkNEsppABaMGOBcsuoLaEUkpSZtEJykxmhuK5JCSqFMbrc79347mMwoS_WTahM22pnuiEUTGVCxlOgInrxB111g3fRXcEYUSJNWQxxjK72VOW7ELyxxcbHB_22oKTY5V38zjvisMc_m9Zs_2WL5TyfM5Apgy-U2H9h</recordid><startdate>201903</startdate><enddate>201903</enddate><creator>Love, D. 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M.</au><au>Venturas, M. D.</au><au>Sperry, J. S.</au><au>Brooks, P. D.</au><au>Pettit, J. L.</au><au>Wang, Y.</au><au>Anderegg, W. R. L.</au><au>Tai, X.</au><au>Mackay, D. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dependence of Aspen Stands on a Subsurface Water Subsidy: Implications for Climate Change Impacts</atitle><jtitle>Water resources research</jtitle><date>2019-03</date><risdate>2019</risdate><volume>55</volume><issue>3</issue><spage>1833</spage><epage>1848</epage><pages>1833-1848</pages><issn>0043-1397</issn><eissn>1944-7973</eissn><abstract>The reliance of 10 Utah (USA) aspen forests on direct infiltration of growing season rain versus an additional subsurface water subsidy was determined from a trait‐ and process‐based model of stomatal control. The model simulated the relationship between water supply to the root zone versus canopy transpiration and assimilation over a growing season. Canopy flux thresholds were identified that distinguished nonstressed, stressed, and dying stands. We found growing season rain and local soil moisture were insufficient for the survival of 5 of 10 stands. Six stands required a substantial subsidy (31–80% of potential seasonal transpiration) to avoid water stress and maximize photosynthetic potential. Subsidy dependence increased with stand hydraulic conductance. Four of the six “subsidized” stands were predicted to be stressed during the survey year owing to a subsidy shortfall. Since winter snowpack is closely related to groundwater recharge in the region, we compared winter precipitation with tree‐ring chronologies. Consistent with model predictions, chronologies were more sensitive to snowpack in subsidized stands than in nonsubsidized ones. The results imply that aspen stand health in the region is more coupled to winter snowpack than to growing season water supply. Winters are predicted to have less precipitation as snow, indicating a stressful future for the region's aspen forests. Key Points Most aspen stands in Utah cannot survive on growing season rain and local soil moisture as their only water supply Aspen stands in Utah are highly dependent on a groundwater subsidy and vulnerable to any subsidy shortfall Aspen stand health in Utah will be threatened by diminished winter snowpack</abstract><cop>Washington</cop><pub>John Wiley &amp; Sons, Inc</pub><doi>10.1029/2018WR023468</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0002-3729-2743</orcidid><orcidid>https://orcid.org/0000-0002-0582-6990</orcidid><orcidid>https://orcid.org/0000-0001-7881-7393</orcidid><orcidid>https://orcid.org/0000-0003-0477-9755</orcidid><orcidid>https://orcid.org/0000-0001-9201-1062</orcidid><orcidid>https://orcid.org/0000-0001-5972-9064</orcidid><orcidid>https://orcid.org/0000-0002-3040-3121</orcidid></addata></record>
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source Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; EZB-FREE-00999 freely available EZB journals
subjects Atmospheric precipitations
Canopies
Canopy
Climate change
Computer simulation
Conductance
Dependence
Environmental impact
Forests
Groundwater
Groundwater recharge
Growing season
growth rings
hydraulic conductivity
Infiltration
Mathematical models
Photosynthesis
plant hydraulics
Precipitation
Predictions
Rain
Resistance
rhizosphere
Root zone
Seasons
snow
Snowpack
Soil
Soil moisture
soil water
Stomata
Subsidies
Subsurface water
subsurface water subsidy
Surveying
surveys
Survival
Transpiration
tree mortality
Utah
Water shortages
Water stress
Water supply
Winter
Winter precipitation
xylem
title Dependence of Aspen Stands on a Subsurface Water Subsidy: Implications for Climate Change Impacts
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