Abstract

Model optimization using data assimilation is an effective tool for reliable projections of environmental changes. To date, however, data assimilation has not been widely applied for terrestrial ecosystem models, especially in large-scale studies, owing to specific difficulties including heterogeneity and abruptness in terrestrial processes. To overcome the difficulties arising from the complex and abrupt behaviour of the terrestrial ecosystem model, the data assimilation by particle filter, a non-parametric and computationally intensive parameter optimization method, was applied in this study. We simultaneously optimized nine model parameters of a terrestrial ecosystem model with a satellite-based leaf area index. The optimized model successfully reproduced the leaf onset and offset phenology of temperate deciduous forests in mainland Japan. We formulated the relationship between local climate and leaf onset and offset timings which indicates that warmer temperatures were required for leaf onset in the warmer southern parts of Japan, and the northern forests retained their leaves under much colder temperatures, relative to southern forests. Unlike the findings of conventional phenology models using crude estimation with limited local data, the results of this study were based on regional big data and objective optimization. This research thus shows that data assimilation can be used to optimize complex terrestrial ecosystem models.

Highlights

  • Terrestrial ecosystems play an important role in the earth system and influence the global climate (Heimann and Reichstein, 2008; Arneth et al, 2010)

  • Stochastic Ecosystem Model (SSSEM) was chosen for this study because it has a built-in data assimilation (DA) system using a particle filter, and its simplicity was desirable for this computer-intensive experiment on a regional scale

  • The simulated dynamics of leaf area index (LAI) were robust against somewhat questionable data

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Summary

Introduction

Terrestrial ecosystems play an important role in the earth system and influence the global climate (Heimann and Reichstein, 2008; Arneth et al, 2010). The terrestrial biosphere is characterized by a two-way feedback process with climate: climatic conditions affect the biosphere, and the biosphere in turn affects the climate by way of biogeochemical and biophysical changes on land surfaces (Arneth et al, 2010). This feedback process is believed to be significant because of terrestrial surface sizes and biogeochemical budgets. The annual cycle of spring leaf onset and fall senescence in temperate deciduous forests is controlled by plant traits, in addition to climatic conditions such as air temperature (White et al, 1997). Understanding how phenological cycles react to climate change is important for decreasing the uncertainty in projections of the terrestrial carbon cycle (Richardson et al, 2012) and elucidating the behaviors of ecosystem dynamics under climate change

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