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Biophysical homoeostasis of leaf temperature: A neglected process for vegetation and land‐surface modelling
Author(s) -
Dong N.,
Prentice I. C.,
Harrison S. P.,
Song Q. H.,
Zhang Y. P.
Publication year - 2017
Publication title -
global ecology and biogeography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.164
H-Index - 152
eISSN - 1466-8238
pISSN - 1466-822X
DOI - 10.1111/geb.12614
Subject(s) - evapotranspiration , environmental science , vegetation (pathology) , atmospheric sciences , canopy , precipitation , air temperature , diurnal cycle , biometeorology , range (aeronautics) , fluxnet , climatology , ecosystem , ecology , geography , meteorology , eddy covariance , biology , medicine , pathology , materials science , composite material , geology
Aim Leaf and air temperatures are seldom equal, but many vegetation models assume that they are. Land‐surface models calculate canopy temperatures, but how well they do so is unknown. We encourage consideration of the leaf‐ and canopy‐to‐air temperature difference (Δ Τ ) as a benchmark for land‐surface modelling and an important feature of plant and ecosystem function. Location Tropical SW China. Time period 2013. Major Taxa studies Tropical trees. Methods We illustrate diurnal cycles of leaf‐ and canopy‐to‐air temperature difference (Δ Τ ) with field measurements in a tropical dry woodland and with continuous monitoring data in a tropical seasonal forest. The Priestley–Taylor (PT) and Penman–Monteith (PM) approaches to evapotranspiration are used to provide insights into the interpretation and prediction of Δ T . Field measurements are also compared with land‐surface model results obtained with the Joint U.K. Land Environment Simulator (JULES) set up for the conditions of the site. Results The Δ T followed a consistent diurnal cycle, with negative values at night (attributable to negative net radiation) becoming positive in the morning, reaching a plateau and becoming negative again when air temperature exceeded a ‘crossover’ in the 24–29 °C range. Daily time courses of Δ T could be approximated by either the PT or the PM model, but JULES tended to underestimate the magnitude of negative Δ T . Main conclusions Leaves with adequate water supply are partly buffered against air‐temperature variations, through a passive biophysical mechanism. This is likely to be important for optimal leaf function, and land‐surface and vegetation models should aim to reproduce it.