Finite element tree crown hydrodynamics model (FETCH) using porous media flow within branching elements: A new representation of tree hydrodynamics

By Gil Bohrer, Hashem M. Mourad, T. Laursen, D. Drewry, R. Avissar, Davide Poggi, Ram Oren, Gabriel G. Katul. 2005

156 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/1160a3a655d8e1afae8338d775a2cbb86873b6bc

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Citations in the corpus

Contrasting strategies of hydraulic control in two codominant temperate tree species (2017, methodology): “A full model description and formulation are provided in Mirfenderesgi et al. (2016) and Bohrer et al. (2005).”
Interdependence of chronic hydraulic dysfunction and canopy processes can improve integrated models of tree response to drought (2015, methodology): “Even models that have profited from the use of plant hydraulics assume immediate recovery of xylem conductance as WS increases [Bohrer et al., 2005; Da Silva et al., 2011; Domec et al., 2012; Hickler et al., 2006; Holtta et al., 2006, 2009; Janott et al., 2010; Magnani et al., 2002; Quijano et al.,…”
Vegetation demographics in Earth System Models: A review of progress and priorities (2018, methodology): “As such, DVMs have historically been tested against these vegetation classification maps (Sitch et al., 2003; Bonan et al., 2003; Arora & Boer 2006; Fisher et al., 2015).”
Xylem embolism refilling and resilience against drought-induced mortality in woody plants: processes and trade-offs (2018, background): “A consideration of hydrodynamics has a long history of development in stand-scale models (e.g. Williams et al. 1996; Bohrer et al. 2005), ecosystem models (Duursma and Medlyn 2012; Christoffersen et al.”
Biological constraints on water transport in the soil–plant–atmosphere system (2013, background): “Water transport in the plant tissues (from the root surface to the leaf cuticle and inner surface of the stomatal cavity) can be treated, in analogy with flow in unsaturated soils, as driven by capillary and gravitational gradients [61,62] as”