“…Stable isotope modeling is not devoid of uncertainties concerning the precision of the approach at short temporal scale, for example, variability of isotopic fractionation factors and within‐plant carbon cycling (Helliker et al., 2018; Sternberg, 2009). Yet, the agreement between isotope‐resolved canopy temperature and eddy covariance measurements confirmed that our current knowledge of the theory provides estimates of T L with satisfying accuracy for broad scales studies encompassing acute climatic variation and multi‐year integrations (Helliker et al., 2018). Since biochemical and physiological parameters used in the tree‐ring cellulose model were originally derived from non‐woody species (e.g., Barbour, Schurr, Henry, Wong, & Farquahr, 2000; Helliker & Ehleringer, 2002; Sternberg, DeNiro, & Savidge, 1986), such modeling approach can be expanded to non‐tree species as well (e.g., Michaletz et al., 2016).…”