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Research article2011Peer reviewed

Analysis of nitrogen controls on carbon and water exchanges in a conifer forest using the CLASS-CTEMN+ model

Huang, Suo; Arain, M. Altaf; Arora, Vivek K.; Yuan, Fengming; Brodeur, Jason; Peichl, Matthias

Abstract

A carbon (C) and nitrogen (N) cycle-coupled model, CLASS-CTEMN+ was developed by incorporating soil and plant N cycling algorithms in the Canadian Land Surface Scheme (CLASS) and the Canadian Terrestrial Ecosystem Model (CTEM), used in the Canadian Global Climate Model. Key soil and plant N cycling processes incorporated in the model include biological fixation, mineralization, nitrification, denitrification, leaching and N controls on plant photosynthesis capacity. The model was used to analyse N controls on C and water exchanges in a 70-year-old temperate conifer forest in southern Ontario, Canada from 2003 to 2007. The simulated values of soil-plant N contents and fluxes - including N2O flux - were generally in good agreement with observations. When N controls on C and water cycling were included in the model, simulated daily gross ecosystem productivity (GEP), ecosystem respiration (R-e), net ecosystem productivity (NEP) and evapotranspiration (ET) fluxes showed improved agreement with eddy covariance flux measurements. The five-year mean annual NEP predicted by the N-coupled model was 121 g C m(-2) yr(-) for 2003-2007, compared to 273 g C m(-2) yr(-1), which was simulated by the model when N controls were switched off (non-N model). N-coupled model estimates compared well with the measured five-year mean (+/- standard deviation) annual NEP of 136 +/- 59 g C m(-2) yr(-1). Simulated annual mean ET over five-years was 384 mm yr(-1) for the N-coupled model, and 433 mm yr(-1) for non-N model, compared with the measured five-year mean annual value of 405 +/- 44 mm yr(-1). Model results confirmed that a proper representation of N controls on photosynthetic uptake and canopy conductance could result in more plausible simulations of observed C and water fluxes. The model results also suggested that N limitations in spring and early summer were generally more important in controlling NEP. Discrepancies between simulated and measured annual variations of C exchanges occurred in years that included extreme weather periods (e.g. low soil water content and warm spring/summer temperatures). (C) 2011 Elsevier B.V. All rights reserved.

Keywords

Nitrogen-Carbon-coupling; Carbon and water fluxes; Temperate forest; Canadian Land Surface Scheme (CLASS); Canadian Terrestrial Ecosystem Model (CTEM)

Published in

Ecological Modelling
2011, Volume: 222, number: 20-22, pages: 3743-3760
Publisher: ELSEVIER SCIENCE BV

    Sustainable Development Goals

    SDG13 Take urgent action to combat climate change and its impacts

    UKÄ Subject classification

    Environmental Sciences related to Agriculture and Land-use

    Publication identifier

    DOI: https://doi.org/10.1016/j.ecolmodel.2011.09.008

    Permanent link to this page (URI)

    https://res.slu.se/id/publ/56979