Forest stand complexity controls ecosystem-scale evapotranspiration dynamics: Implications for landscape flux simulations

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dc.contributor.authorLeonard, Rhoswen
dc.contributor.authorMoore, Paul
dc.contributor.authorKrause, Stefan
dc.contributor.authorChasmer, Laura
dc.contributor.authorDevito, Kevin J.
dc.contributor.authorPetrone, Richard M.
dc.contributor.authorMendoza, Carl
dc.contributor.authorWaddington, James M.
dc.contributor.authorKettridge, Nicholas
dc.date.accessioned2024-08-20T19:25:42Z
dc.date.available2024-08-20T19:25:42Z
dc.date.issued2022
dc.descriptionOpen access article. Creative Commons Attribution 4.0 International license (CC BY 4.0) applies
dc.description.abstractOpen-canopy forested systems are found across a range of terrestrial biomes. Forest structure and organization in open-canopy systems exhibit substantial controls on system process dynamics such as evapotranspiration (ET). The energy reaching sub-canopy forest layers is greater in open-canopy systems compared to closed canopy systems, with high spatiotemporal variability in the distribution of energy that both drives ET and controls sub canopy species composition and organization. Yet the impact of their structural complexity and organization on whole system ET dynamics is poorly understood. Using the BETA+ model and measured eddy covariance-based ET fluxes from a boreal treed peatland, we critically evaluate how stand compositional and organizational complexity influences ET dynamics. Model simulations iteratively increase complexity from a simple ‘big-leaf’ model to a model representing spatial complexity of all system layers, demonstrating the effect of each complex system component on stand ET dynamics. We show that including forest stand complexity and associated canopy and radiation variability increases ET model estimates by ~26%. In addition to changes in the ET estimates, the inclusion of this spatial complexity is shown to induce temporal variations in the simulated ET that improves model performance by reducing unexplained variance between modelled and measured ET by 10% and reducing hysteresis in model results. These results have clear implications for flux modelling of forest systems and for larger scale climate models where open canopy systems such as this dominate the landscape. Demonstrating that whilst big leaf simulation can approximate ET fluxes, the inclusion of forest-stand complexity and its influence on spatiotemporal radiation fluxes and ecohydrological processes are necessary to effectively represent ET dynamics within open canopies.
dc.description.peer-reviewYes
dc.identifier.citationLeonard, R., Moore, P., Krause, S., Chasmer, L., Devito, K. J., Petrone, R. M., Mendoza, C., Waddington, J. M., & Kettridge, N. (2022). Forest stand complexity controls ecosystem-scale evapotranspiration dynamics: Implications for landscape flux simulations. Hydrological Processes, 36(12), Article e14761. https://doi.org/10.1002/hyp.14761
dc.identifier.urihttps://hdl.handle.net/10133/6871
dc.language.isoen
dc.publisherWiley
dc.publisher.departmentDepartment of Geography and Environment
dc.publisher.facultyArts and Science
dc.publisher.institutionUniversity of Birmingham
dc.publisher.institutionMcMaster University
dc.publisher.institutionUniversity of Lethbridge
dc.publisher.institutionUniversity of Alberta
dc.publisher.institutionUniversity of Waterloo
dc.publisher.urlhttps://doi.org/10.1002/hyp.14761
dc.subjectBoreal forest
dc.subjectEddy covariance
dc.subjectEvapotranspiration
dc.subjectModelling
dc.subjectPeatland
dc.subjectOpen canopy forests
dc.subjectForest stand
dc.subject.lcshPeatland forestry
dc.subject.lcshTaigas
dc.titleForest stand complexity controls ecosystem-scale evapotranspiration dynamics: Implications for landscape flux simulations
dc.typeArticle
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