Abstract
Abstract. Natural and anthropogenic disturbances, in particular forest management, affect forest age structures all around the globe. Forest age structures in turn influence key land surface processes, such as photosynthesis and thus the carbon cycle. Yet, many dynamic global vegetation models (DGVMs), including those used as land surface models (LSMs) in Earth system models (ESMs), do not account for subgrid forest age structures, despite being used to investigate land-use effects on the global carbon budget or simulating biogeochemical responses to climate change. In this paper we present a new scheme to introduce forest age classes in hierarchical tile-based DGVMs combining benefits of recently applied approaches the first being a computationally efficient age-dependent simulation of all relevant processes, such as photosynthesis and respiration, using a restricted number of age classes and the second being the tracking of the exact forest age, which is a prerequisite for any implementation of age-based forest management. This combination is achieved by using the tile hierarchy to track the area fraction for each age on an aggregated plant functional type level, whilst simulating the relevant processes for a set of age classes. We describe how we implemented this scheme in JSBACH4, the LSM of the ICOsahedral Non-hydrostatic Earth system model (ICON-ESM). Subsequently, we compare simulation output to global observation-based products for gross primary production, leaf area index, and above-ground biomass to assess the ability of simulations with and without age classes to reproduce the annual cycle and large-scale spatial patterns of these variables. The comparisons show decreasing differences and increasing computation costs with an increasing number of distinguished age classes. The results demonstrate the benefit of the introduction of age classes, with the optimal number of age classes being a compromise between computation costs and error reduction.
Highlights
Land use, forest management, substantially influences the age structure of global forests (Pan et al, 2011; Erb et al, 2017)
Having forest age classes in JSBACH4–FF facilitates a finer discretisation in each grid cell and is a precondition for any implementation of age-based forest management
The number of age classes in JSBACH4–FF is flexible, and in the following we describe the evaluation of simulation results using different numbers of age classes and age distribution schemes and discuss the compromise between computation costs and error reduction, when selecting a certain number of age classes (Sect. 3.1)
Summary
Forest management, substantially influences the age structure of global forests (Pan et al, 2011; Erb et al, 2017). More than 19 Mkm of forest area, i.e. about 15 % of global ice-free land, are under some kind of management (Luyssaert et al, 2014), with 65 % being under regular harvest schemes and another 7 % being intensive plantations (Erb et al, 2017). Forest age structures are influenced by other natural or anthropogenically caused disturbances such as fires, windthrows, droughts, pests, and insect outbreaks Changes in forest age structure in turn influence biophysical and biogeochemical interactions with the atmosphere, through changes in land surface properties such as albedo and carbon uptake
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