Ecohydrological modelling with EcH2O-iso to quantify forest and grassland effects on water partitioning and flux ages

Audrey Douinot (Corresponding Author), Doerthe Tetzlaff, Marco Maneta, Sylvain Kuppel, Hubert Schulte-Bisping, Chris Soulsby

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

We used the new process-based, tracer-aided ecohydrological model EcH(2)O-iso to assess the effects of vegetation cover on water balance partitioning and associated flux ages under temperate deciduous beech forest (F) and grassland (G) at an intensively monitored site in Northern Germany. Unique, multicriteria calibration, based on measured components of energy balance, hydrological function and biomass accumulation, resulted in good simulations reproducing measured soil surface temperatures, soil water content, transpiration, and biomass production. Model results showed the forest "used" more water than the grassland; of 620 mm average annual precipitation, losses were higher through interception (29% under F, 16% for G) and combined soil evaporation and transpiration (59% F, 47% G). Consequently, groundwater (GW) recharge was enhanced under grassland at 37% (similar to 225 mm) of precipitation compared with 12% (similar to 73 mm) for forest. The model tracked the ages of water in different storage compartments and associated fluxes. In shallow soil horizons, the average ages of soil water fluxes and evaporation were similar in both plots (similar to 1.5 months), though transpiration and GW recharge were older under forest (similar to 6 months compared with similar to 3 months for transpiration, and similar to 12 months compared with similar to 10 months for GW). Flux tracking using measured chloride data as a conservative tracer provided independent support for the modelling results, though highlighted effects of uncertainties in forest partitioning of evaporation and transpiration. By tracking storage-flux-age interactions under different land covers, EcH(2)O-iso could quantify the effects of vegetation on water partitioning and age distributions. Given the likelihood of drier, warmer summers, such models can help assess the implications of land use for water resource availability to inform debates over building landscape resilience to climate change. Better conceptualization of soil water mixing processes and improved calibration data on leaf area index and root distribution appear obvious respective modelling and data needs for improved simulations.

Original languageEnglish
Pages (from-to)2174-2191
Number of pages18
JournalHydrological Processes
Volume33
Issue number16
Early online date19 Jun 2019
DOIs
Publication statusPublished - 30 Jul 2019

Fingerprint

transpiration
partitioning
grassland
evaporation
modeling
soil water
groundwater
recharge
water
tracer
calibration
shallow soil
biomass
resource availability
soil horizon
interception
temperate forest
deciduous forest
leaf area index
age structure

Keywords

  • forest hydrology
  • ecohydrology
  • tracers
  • tracer-aided models
  • CARBON
  • CLIMATE-CHANGE
  • TRANSPIRATION
  • VARIABILITY
  • LAND-USE CHANGE
  • STORAGE DYNAMICS
  • GLOBAL SYNTHESIS
  • PANOLA MOUNTAIN
  • LEAF-AREA INDEX
  • VEGETATION

ASJC Scopus subject areas

  • Water Science and Technology

Cite this

Ecohydrological modelling with EcH2O-iso to quantify forest and grassland effects on water partitioning and flux ages. / Douinot, Audrey (Corresponding Author); Tetzlaff, Doerthe; Maneta, Marco; Kuppel, Sylvain; Schulte-Bisping, Hubert; Soulsby, Chris.

In: Hydrological Processes, Vol. 33, No. 16, 30.07.2019, p. 2174-2191.

Research output: Contribution to journalArticle

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author = "Audrey Douinot and Doerthe Tetzlaff and Marco Maneta and Sylvain Kuppel and Hubert Schulte-Bisping and Chris Soulsby",
note = "ACKNOWLEDGMENTS The authors would like to acknowledge research funding from the European Research Council (project GA 335910 VeWa). M. Maneta acknowledges support from the U.S. National Science Foundation (project GSS 1461576). C. S. is grateful to the Leibniz IGB Berlin for a Senior Research Fellowship. We also thank Umweltbundesamt (UBA) for providing the climate data. DATA AVAILABILITY STATEMENT The data that support the findings of this study are available from the corresponding author upon reasonable request.",
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AU - Douinot, Audrey

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AU - Kuppel, Sylvain

AU - Schulte-Bisping, Hubert

AU - Soulsby, Chris

N1 - ACKNOWLEDGMENTS The authors would like to acknowledge research funding from the European Research Council (project GA 335910 VeWa). M. Maneta acknowledges support from the U.S. National Science Foundation (project GSS 1461576). C. S. is grateful to the Leibniz IGB Berlin for a Senior Research Fellowship. We also thank Umweltbundesamt (UBA) for providing the climate data. DATA AVAILABILITY STATEMENT The data that support the findings of this study are available from the corresponding author upon reasonable request.

PY - 2019/7/30

Y1 - 2019/7/30

N2 - We used the new process-based, tracer-aided ecohydrological model EcH(2)O-iso to assess the effects of vegetation cover on water balance partitioning and associated flux ages under temperate deciduous beech forest (F) and grassland (G) at an intensively monitored site in Northern Germany. Unique, multicriteria calibration, based on measured components of energy balance, hydrological function and biomass accumulation, resulted in good simulations reproducing measured soil surface temperatures, soil water content, transpiration, and biomass production. Model results showed the forest "used" more water than the grassland; of 620 mm average annual precipitation, losses were higher through interception (29% under F, 16% for G) and combined soil evaporation and transpiration (59% F, 47% G). Consequently, groundwater (GW) recharge was enhanced under grassland at 37% (similar to 225 mm) of precipitation compared with 12% (similar to 73 mm) for forest. The model tracked the ages of water in different storage compartments and associated fluxes. In shallow soil horizons, the average ages of soil water fluxes and evaporation were similar in both plots (similar to 1.5 months), though transpiration and GW recharge were older under forest (similar to 6 months compared with similar to 3 months for transpiration, and similar to 12 months compared with similar to 10 months for GW). Flux tracking using measured chloride data as a conservative tracer provided independent support for the modelling results, though highlighted effects of uncertainties in forest partitioning of evaporation and transpiration. By tracking storage-flux-age interactions under different land covers, EcH(2)O-iso could quantify the effects of vegetation on water partitioning and age distributions. Given the likelihood of drier, warmer summers, such models can help assess the implications of land use for water resource availability to inform debates over building landscape resilience to climate change. Better conceptualization of soil water mixing processes and improved calibration data on leaf area index and root distribution appear obvious respective modelling and data needs for improved simulations.

AB - We used the new process-based, tracer-aided ecohydrological model EcH(2)O-iso to assess the effects of vegetation cover on water balance partitioning and associated flux ages under temperate deciduous beech forest (F) and grassland (G) at an intensively monitored site in Northern Germany. Unique, multicriteria calibration, based on measured components of energy balance, hydrological function and biomass accumulation, resulted in good simulations reproducing measured soil surface temperatures, soil water content, transpiration, and biomass production. Model results showed the forest "used" more water than the grassland; of 620 mm average annual precipitation, losses were higher through interception (29% under F, 16% for G) and combined soil evaporation and transpiration (59% F, 47% G). Consequently, groundwater (GW) recharge was enhanced under grassland at 37% (similar to 225 mm) of precipitation compared with 12% (similar to 73 mm) for forest. The model tracked the ages of water in different storage compartments and associated fluxes. In shallow soil horizons, the average ages of soil water fluxes and evaporation were similar in both plots (similar to 1.5 months), though transpiration and GW recharge were older under forest (similar to 6 months compared with similar to 3 months for transpiration, and similar to 12 months compared with similar to 10 months for GW). Flux tracking using measured chloride data as a conservative tracer provided independent support for the modelling results, though highlighted effects of uncertainties in forest partitioning of evaporation and transpiration. By tracking storage-flux-age interactions under different land covers, EcH(2)O-iso could quantify the effects of vegetation on water partitioning and age distributions. Given the likelihood of drier, warmer summers, such models can help assess the implications of land use for water resource availability to inform debates over building landscape resilience to climate change. Better conceptualization of soil water mixing processes and improved calibration data on leaf area index and root distribution appear obvious respective modelling and data needs for improved simulations.

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KW - tracers

KW - tracer-aided models

KW - CARBON

KW - CLIMATE-CHANGE

KW - TRANSPIRATION

KW - VARIABILITY

KW - LAND-USE CHANGE

KW - STORAGE DYNAMICS

KW - GLOBAL SYNTHESIS

KW - PANOLA MOUNTAIN

KW - LEAF-AREA INDEX

KW - VEGETATION

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JO - Hydrological Processes

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SN - 0885-6087

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