Precipitation mediates sap flux sensitivity to evaporative demand in the neotropics

Authors

Charlotte Grossiord, Eidgenössische Forschungsanstalt für Wald, Schnee und Landschaft WSL
Bradley Christoffersen, The University of Texas Rio Grande Valley
Aura M. Alonso-Rodríguez, USDA Forest Service
Kristina Anderson-Teixeira, Smithsonian Tropical Research Institute
Heidi Asbjornsen, University of New Hampshire Durham
Luiza Maria T. Aparecido, School of Life Sciences
Z. Carter Berry, Chapman University
Christopher Baraloto, Florida International University
Damien Bonal, Université de Lorraine
Isaac Borrego, Los Alamos National Laboratory
Benoit Burban, Université des Antilles
Jeffrey Q. Chambers, University of California, Berkeley
Danielle S. Christianson, Lawrence Berkeley National Laboratory
Matteo Detto, Princeton University
Boris Faybishenko, University of California, Berkeley
Clarissa G. Fontes, University of California, Berkeley
Claire Fortunel, The University of Texas at Austin
Bruno O. Gimenez, Instituto Nacional de Pesquisas Da Amazonia
Kolby J. Jardine, Lawrence Berkeley National Laboratory
Lara Kueppers, University of California, Berkeley
Gretchen R. Miller, College of Engineering
Georgianne W. Moore, Texas A&M University
Robinson Negron-Juarez, University of California, Berkeley
Clément Stahl, Université des Antilles
Nathan G. Swenson, College of Computer, Mathematical, & Natural Sciences
Volodymyr Trotsiuk, Eidgenössische Forschungsanstalt für Wald, Schnee und Landschaft WSL
Charu Varadharajan, University of California, Berkeley
Jeffrey M. Warren, ORNL Environmental Sciences Division
Brett T. Wolfe, Smithsonian Tropical Research Institute
Liang Wei, Los Alamos National Laboratory
Tana E. Wood, USDA Forest Service
Chonggang Xu, Los Alamos National Laboratory
Nate G. McDowell, Pacific Northwest National Laboratory

Document Type

Article

Publication Date

11-1-2019

Abstract

Transpiration in humid tropical forests modulates the global water cycle and is a key driver of climate regulation. Yet, our understanding of how tropical trees regulate sap flux in response to climate variability remains elusive. With a progressively warming climate, atmospheric evaporative demand [i.e., vapor pressure deficit (VPD)] will be increasingly important for plant functioning, becoming the major control of plant water use in the twenty-first century. Using measurements in 34 tree species at seven sites across a precipitation gradient in the neotropics, we determined how the maximum sap flux velocity (vmax) and the VPD threshold at which vmax is reached (VPDmax) vary with precipitation regime [mean annual precipitation (MAP); seasonal drought intensity (PDRY)] and two functional traits related to foliar and wood economics spectra [leaf mass per area (LMA); wood specific gravity (WSG)]. We show that, even though vmax is highly variable within sites, it follows a negative trend in response to increasing MAP and PDRY across sites. LMA and WSG exerted little effect on vmax and VPDmax, suggesting that these widely used functional traits provide limited explanatory power of dynamic plant responses to environmental variation within hyper-diverse forests. This study demonstrates that long-term precipitation plays an important role in the sap flux response of humid tropical forests to VPD. Our findings suggest that under higher evaporative demand, trees growing in wetter environments in humid tropical regions may be subjected to reduced water exchange with the atmosphere relative to trees growing in drier climates.

Publication Source (Journal or Book title)

Oecologia

First Page

519

Last Page

530

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