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Temporal changes in global soil respiration since 1987.

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Soil respiration (Rs) initially increased with climate warming but later stabilized globally. Despite this, microbial decomposition (Rh) suggests ongoing soil carbon loss, potentially indicating a future rise in Rs.

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Area of Science:

  • Earth and Environmental Sciences
  • Climate Science
  • Soil Science

Background:

  • Soil respiration (Rs) is a major terrestrial carbon flux significantly influenced by climate warming.
  • Uncertainty in the global scale and dynamics of Rs stimulation challenges climate projection accuracy.

Purpose of the Study:

  • To analyze global Rs observations from 1987-2016 to understand its temporal dynamics and response to climate change.
  • To investigate the relationship between temperature anomalies, soil carbon stocks, and Rs variations.

Main Methods:

  • Analysis of global soil respiration (Rs) observations spanning from 1987 to 2016.
  • Examination of temporal variations in temperature anomalies and soil carbon (C) stocks.
  • Modeling analysis to predict potential future trends in global Rs.

Main Results:

  • Global Rs increased significantly from 1987-1999 but stabilized between 2000-2016.
  • Global heterotrophic respiration (Rh) consistently increased from 1987-2016, indicating accumulated soil C losses.
  • Recent warming trends suggest a potential resurgence of global Rs increase.

Conclusions:

  • Observed shifts in Rs provide critical data for understanding carbon cycle responses to climate change.
  • Findings offer insights for developing effective climate change mitigation policies.
  • The study highlights the complex interplay between warming, soil carbon, and respiration.