Different Responses of Terrestrial Carbon Fluxes to Environmental Changes in Cold Temperate Forest Ecosystems

• Published in: Forests 2024-08, Vol.15 (8), p.1340
• Main Authors: Jiang, Mihang, Liu, Xinjie, Liu, Liangyun
• Format: Article
• Language: English
• Subjects: Annual precipitation; Autumn; Brittleness; carbon; Carbon cycle; Carbon cycle (Biogeochemistry); Carbon dioxide; Carbon sequestration; Carbon sinks; China; Climatic changes; Cold; Correlation coefficient; Correlation coefficients; Datasets; Decoupling; ecosystem respiration; Environmental aspects; Environmental changes; Environmental conditions; Environmental factors; Fluxes; Forecasts and trends; Forest ecosystems; Forests; Forests and forestry; global carbon budget; gross primary productivity; Least squares method; net ecosystem production; path analysis; photosynthesis; Precipitation; Productivity; Radiation; Respiration; Short wave radiation; shortwave radiation; Spring; Spring (season); Statistical analysis; Summer; Temperate forests; temperate zones; Temperature; Terrestrial ecosystems; Time series; Trends; Vapor pressure; vapor pressure deficit; Variables; Vegetation
• ISSN: 1999-4907; 1999-4907
• DOI: 10.3390/f15081340

As the largest carbon reservoir within terrestrial ecosystems, forest ecosystems play a major role as carbon sinks in the global carbon cycle. There are still some uncertainties regarding the responses of different carbon fluxes to environmental changes in cold temperate climate forest ecosystems. Here, 14 cold temperate forest flux sites for at least ten years were investigated, including carbon fluxes and environmental variables such as temperature, precipitation, shortwave radiation, and vapor pressure deficit. By calculating the Spearman correlation coefficient, there was a congruence between photosynthetic productivity (i.e., gross primary productivity, GPP) and carbon sequestration (i.e., net ecosystem productivity, NEP) at thirteen forest sites, and at one forest site, GPP and NEP were decoupled. Annual GPP and NEP displayed a consistent trend when temperature and precipitation had significantly opposite trends and when temperature had a significantly positive correlation with VPD. But when VPD was significantly negatively correlated with both temperature and SW in spring and when temperature was negatively correlated with both SW and VPD in summer, a decoupling of GPP and NEP occurred. The impacts of various environmental factors on the annual carbon fluxes were calculated for each year and season using the path analysis method. At forest sites with consistent trends in GPP and NEP, annual, spring, and summer temperatures had significant positive correlations with GPP and ecosystem respiration (RE). While at the decoupled forest site, environmental factors had a stronger effect on RE, which then contributed to the observed decoupling of GPP and NEP. Finally, the Partial Least Squares method was used to analyze the relative contribution of each environmental factor to annual carbon fluxes. The results revealed that temperature and summer precipitation were the key environmental factors affecting forest ecosystems. This study provides important insights into the different responses of carbon fluxes in forest ecosystems undergoing environmental changes.