Abstract

AbstractLeaf maintenance respiration (Rleaf,m) is a major but poorly understood component of the terrestrial carbon cycle (C). Earth systems models (ESMs) use simple sub‐models relating Rleaf,m to leaf traits, applied at canopy scale. Rleaf,m models vary depending on which leaf N traits they incorporate (e.g., mass or area based) and the form of relationship (linear or nonlinear). To simulate vegetation responses to global change, some ESMs include ecological optimization to identify canopy structures that maximize net C accumulation. However, the implications for optimization of using alternate leaf‐scale empirical Rleaf,m models are undetermined. Here we combine alternate well‐known empirical models of Rleaf,m with a process model of canopy photosynthesis. We quantify how net canopy exports of C vary with leaf area index (LAI) and total canopy N (TCN). Using data from tropical and arctic canopies, we show that estimates of canopy Rleaf,m vary widely among the three models. Using an optimization framework, we show that the LAI and TCN values maximizing C export depends strongly on the Rleaf,m model used. No single model could match observed arctic and tropical LAI‐TCN patterns with predictions of optimal LAI‐TCN. We recommend caution in using leaf‐scale empirical models for components of ESMs at canopy‐scale. Rleaf,m models may produce reasonable results for a specified LAI, but, due to their varied representations of Rleaf,mfoliar N sensitivity, are associated with different and potentially unrealistic optimization dynamics at canopy scale. We recommend ESMs to be evaluated using response surfaces of canopy C export in LAI‐TCN space to understand and mitigate these risks.

Highlights

  • Respiration by leaves (Rleaf) is a major component of the global carbon (C) cycle

  • Patterns in Canopy Respiration Across Observed leaf area index (LAI) and total canopy N (TCN) for Differing Leaf Respiration Models The three Rleaf,m models have clear differences in their response surfaces when visualized in LAI‐TCN phase spaces (Figure 2)

  • We learn that none of the Rleaf,m models produced upscaled estimates of respiration that were economically consistent across all the canopy types we investigated, and we reject our hypothesis on model complexity

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Summary

Introduction

Respiration by leaves (Rleaf) is a major component of the global carbon (C) cycle. Rleaf has been estimated to comprise ~50% of total autotrophic respiration, which is the largest contribution of any plant tissue (Atkin et al, 2007), and represents ~30‐Gt C released globally by terrestrial ecosystems per year (Atkin et al, 2017), a flux much larger than current fossil fuel emissions. Journal of Advances in Modeling Earth Systems has been estimated to account for 43% of total (vegetation and soils) respiration in a tropical forest (Cavaleri et al, 2017), greater than any other component (soils, live wood, and woody debris). Predicting the dynamics of Rleaf across biomes is critical for simulating current and future global C cycling. While detailed and robust biochemical models of photosynthesis exist that are applied globally (Farquhar & von Caemmerer, 1982), an equivalent for leaf maintenance respiration is lacking

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