Coupled modeling of peatlands carbon cycle and carbon dioxide emission from their peat deposits

Abstract COmplex Model of BOg LAndscapes (COMBOLA) is a set of dynamic models of carbon and nitrogen turnover, net ecosystem exchange, water balance, heat and water transport, generation and transfer of CO 2 and CH 4 in a peat deposit on a number of time scales. Combined modeling of carbon turnover...

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Bibliographic Details
Published in:IOP Conference Series: Earth and Environmental Science
Main Author: Zavalishin, N N
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2022
Subjects:
Online Access:http://dx.doi.org/10.1088/1755-1315/1093/1/012009
https://iopscience.iop.org/article/10.1088/1755-1315/1093/1/012009
https://iopscience.iop.org/article/10.1088/1755-1315/1093/1/012009/pdf
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Summary:Abstract COmplex Model of BOg LAndscapes (COMBOLA) is a set of dynamic models of carbon and nitrogen turnover, net ecosystem exchange, water balance, heat and water transport, generation and transfer of CO 2 and CH 4 in a peat deposit on a number of time scales. Combined modeling of carbon turnover and carbon dioxide emission from peat deposits on an annual time scale is carried out as part of COMBOLA for several bog landscapes in Western-Siberian south taiga. One-dimensional vertical reaction-diffusion model for carbon dioxide emission from peat deposit is combined with compartment carbon cycle model allowing estimate both bog type vegetation changes and greenhouse gases balance under probable climate change or perturbations initiated by human activities. Water table level (WTL) separating aerobic peat layer from the anaerobic one is calculated by means of the whole peat layer depth and its water balance relations. Minimal statistical information is used for calibrating temperature dependencies together with coefficients of heat and water transfer equations. The stationary states of carbon cycle are accompanied by steady average profiles of carbon dioxide concentration and can loose stability under human or climatic perturbations. The model dynamics is simulated with several climatic projections of the IPSL atmospheric circulation model for 21 st century with anthropogenic scenarios RCP-2.6 and RCP-8.5.