Discussion
Leaf longevity and turnover rate have been used by LPJ to calculate several key processes of ecosystem carbon cycle. Many previous studies have reported significant correlations between leaf longevity and many other leaf structural and physiological properties such as leaf photosynthetic assimilation rate, leaf nitrogen and specific leaf area (SLA) (Wright, Thornton, Running, & Nemani, 2000; Wright et al., 2004; Reich, Wright, & Lusk, 2007). LPJ employed an empirical relationship derived by Reich et al. (1997) relating SLA to leaf longevity (Eq. 1). Because SLA was used to calculate the leaf area index (LAI) and foliage projective cover (FPC), leaf longevity would further determine the vegetation dynamics, plant photosynthesis and respiration (Koike, 1987; Matsuki and Koike 2006). The leaf turnover rate in LPJ was used to calculate the annual litter input, as well as to determine the size of the canopy biomass, the substrate of heterotrophic respiration (Hikosaka, 2005). Overall, leaf longevity and turnoverrate are involved inmany key variables and processes in LPJ.