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Rainfall drives variation in rates of change in intrinsic water use efficiency of tropical forests.


ABSTRACT: Rates of change in intrinsic water use efficiency (W) of trees relative to those in atmospheric [CO2] (ca) have been mostly assessed via short-term studies (e.g., leaf analysis, flux analysis) and/or step increases in ca (e.g., FACE studies). Here we use compiled data for abundances of carbon isotopes in tree stems to show that on decadal scales, rates of change (dW/dca) vary with location and rainfall within the global tropics. For the period 1915-1995, and including corrections for mesophyll conductance and photorespiration, dW/dca for drier tropical forests (receiving ~?1000?mm rainfall) were at least twice that of the wettest (receiving ~?4000?mm). The data also empirically confirm theorized roles of tropical forests in changes in atmospheric 13C/12C ratios (the 13C Suess Effect). Further formal analysis of geographic variation in decade-to-century scale dW/dca will be needed to refine current models that predict increases in carbon uptake by forests without hydrological cost.

SUBMITTER: Adams MA 

PROVIDER: S-EPMC6694106 | biostudies-literature | 2019 Aug

REPOSITORIES: biostudies-literature

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Rainfall drives variation in rates of change in intrinsic water use efficiency of tropical forests.

Adams Mark A MA   Buckley Thomas N TN   Turnbull Tarryn L TL  

Nature communications 20190814 1


Rates of change in intrinsic water use efficiency (W) of trees relative to those in atmospheric [CO<sub>2</sub>] (c<sub>a</sub>) have been mostly assessed via short-term studies (e.g., leaf analysis, flux analysis) and/or step increases in c<sub>a</sub> (e.g., FACE studies). Here we use compiled data for abundances of carbon isotopes in tree stems to show that on decadal scales, rates of change (dW/dc<sub>a</sub>) vary with location and rainfall within the global tropics. For the period 1915-199  ...[more]

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