Timing of the compensation of winter respiratory carbon losses provides explanatory power for net ecosystem productivity of forests

  • M. Haeni
  • , R. Zweifel
  • , W. Eugster
  • , A. Gessler
  • , S. Zielis
  • , C. Bernhofer
  • , A. Carrara
  • , T. Grünwald
  • , K. Havránková
  • , B. Heinesch
  • , M. Herbst
  • , Andreas Ibrom
  • , A. Knohl
  • , F. Lagergren
  • , B. E. Law
  • , M. Marek
  • , G. Matteucci
  • , J. H. McCaughey
  • , S. Minerbi
  • , L. Montagnani
  • E. Moors, J. Olejnik, M. Pavelka, Kim Pilegaard, G. Pita, A. Rodrigues, M. J. Sanz Sánchez, M.-J. Schelhaas, M. Urbaniak, R. Valentini, A. Varlagin, T. Vesala, C. Vincke, J. Wu, N. Buchmann

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    Abstract

    Accurate predictions of net ecosystem productivity (NEPc) of forest ecosystems are essential for climate change decisions and requirements in the context of national forest growth and greenhouse gas inventories. However, drivers and underlying mechanisms determining NEPc (e.g. climate, nutrients) are not entirely understood yet, particularly when considering the influence of past periods.

    Here we explored the explanatory power of the compensation day (cDOY) —defined as the day of year when winter net carbon losses are compensated by spring assimilation— for NEPc in 26 forests in Europe, North America, and Australia, using different NEPc integration methods.

    We found cDOY to be a particularly powerful predictor for NEPc of temperate evergreen needle-leaf forests (R2 = 0.58) and deciduous broadleaf forests (R2 = 0.68). In general, the latest cDOY correlated with the lowest NEPc. The explanatory power of cDOY depended on the integration method for NEPc, forest type, and whether the site had a distinct winter net respiratory carbon loss or not. The integration methods starting in autumn led to better predictions of NEPc from cDOY then the classical calendar method starting at January 1. Limited explanatory power of cDOY for NEPc was found for warmer sites with no distinct winter respiratory loss period.

    Our findings highlight the importance of the influence of winter processes and the delayed responses of previous seasons’ climatic conditions on current year's NEPc. Such carry-over effects may contain information from climatic conditions, carbon storage levels and hydraulic traits of several years back in time.
    Original languageEnglish
    JournalJournal of Geophysical Research: Biogeosciences
    Volume122
    Issue number1
    Pages (from-to)243-260
    ISSN2169-8953
    DOIs
    Publication statusPublished - 2017

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 13 - Climate Action
      SDG 13 Climate Action

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