Statistical upscaling of ecosystem CO₂ fluxes across the terrestrial tundra and boreal domain : Regional patterns and uncertainties

Summary, in English

The regional variability in tundra and boreal carbon dioxide (CO₂) fluxes can be high, complicating efforts to quantify sink-source patterns across the entire region. Statistical models are increasingly used to predict (i.e., upscale) CO₂ fluxes across large spatial domains, but the reliability of different modeling techniques, each with different specifications and assumptions, has not been assessed in detail. Here, we compile eddy covariance and chamber measurements of annual and growing season CO₂ fluxes of gross primary productivity (GPP), ecosystem respiration (ER), and net ecosystem exchange (NEE) during 1990–2015 from 148 terrestrial high-latitude (i.e., tundra and boreal) sites to analyze the spatial patterns and drivers of CO₂ fluxes and test the accuracy and uncertainty of different statistical models. CO₂ fluxes were upscaled at relatively high spatial resolution (1 km²) across the high-latitude region using five commonly used statistical models and their ensemble, that is, the median of all five models, using climatic, vegetation, and soil predictors. We found the performance of machine learning and ensemble predictions to outperform traditional regression methods. We also found the predictive performance of NEE-focused models to be low, relative to models predicting GPP and ER. Our data compilation and ensemble predictions showed that CO₂ sink strength was larger in the boreal biome (observed and predicted average annual NEE −46 and −29 g C m⁻² yr⁻¹, respectively) compared to tundra (average annual NEE +10 and −2 g C m⁻² yr⁻¹). This pattern was associated with large spatial variability, reflecting local heterogeneity in soil organic carbon stocks, climate, and vegetation productivity. The terrestrial ecosystem CO₂ budget, estimated using the annual NEE ensemble prediction, suggests the high-latitude region was on average an annual CO₂ sink during 1990–2015, although uncertainty remains high.

• Författare: Anna Maria Virkkala; Juha Aalto; Brendan M. Rogers; Torbern Tagesson; Claire C. Treat; Susan M. Natali; Jennifer D. Watts; Stefano Potter; Aleksi Lehtonen; Marguerite Mauritz; Edward A.G. Schuur; John Kochendorfer; Donatella Zona; Walter Oechel; Hideki Kobayashi; Elyn Humphreys; Mathias Goeckede; Hiroki Iwata; Peter M. Lafleur; Eugenie S. Euskirchen; Stef Bokhorst; Maija Marushchak; Pertti J. Martikainen; Bo Elberling; Carolina Voigt; Christina Biasi; Oliver Sonnentag; Frans Jan W. Parmentier; Masahito Ueyama; Gerardo Celis; Vincent L. St.Louis; Craig A. Emmerton; Matthias Peichl; Jinshu Chi; Järvi Järveoja; Mats B. Nilsson; Steven F. Oberbauer; Margaret S. Torn; Sang Jong Park; Han Dolman; Ivan Mammarella; Namyi Chae; Rafael Poyatos; Efrén López-Blanco; Torben Røjle Christensen; Min Jung Kwon; Torsten Sachs; David Holl; Miska Luoto
• Avdelning/ar: Institutionen för naturgeografi och ekosystemvetenskap; BECC: Biodiversity and Ecosystem services in a Changing Climate; MERGE: ModElling the Regional and Global Earth system
• Publiceringsår: 2021
• Språk: Engelska
• Sidor: 4040-4059
• Publikation/Tidskrift/Serie: Global Change Biology
• Volym: 27
• Issue: 17
• Länkar: http://dx.doi.org/10.1111/gcb.15659
• Dokumenttyp: Artikel i tidskrift
• Förlag: Wiley-Blackwell
• Ämne: Earth and Related Environmental Sciences
• Nyckelord: Arctic; CO balance; empirical; greenhouse gas; land; permafrost; remote sensing
• Status: Published
• ISBN/ISSN/Övrigt: ISSN: 1354-1013