Biogeosciences (Jan 2016)

The carbon cycle in Mexico: past, present and future of C stocks and fluxes

  • G. Murray-Tortarolo,
  • P. Friedlingstein,
  • S. Sitch,
  • V. J. Jaramillo,
  • F. Murguía-Flores,
  • A. Anav,
  • Y. Liu,
  • A. Arneth,
  • A. Arvanitis,
  • A. Harper,
  • A. Jain,
  • E. Kato,
  • C. Koven,
  • B. Poulter,
  • B. D. Stocker,
  • A. Wiltshire,
  • S. Zaehle,
  • N. Zeng

DOI
https://doi.org/10.5194/bg-13-223-2016
Journal volume & issue
Vol. 13, no. 1
pp. 223 – 238

Abstract

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We modeled the carbon (C) cycle in Mexico with a process-based approach. We used different available products (satellite data, field measurements, models and flux towers) to estimate C stocks and fluxes in the country at three different time frames: present (defined as the period 2000–2005), the past century (1901–2000) and the remainder of this century (2010–2100). Our estimate of the gross primary productivity (GPP) for the country was 2137 ± 1023 TgC yr−1 and a total C stock of 34 506 ± 7483 TgC, with 20 347 ± 4622 TgC in vegetation and 14 159 ± 3861 in the soil.Contrary to other current estimates for recent decades, our results showed that Mexico was a C sink over the period 1990–2009 (+31 TgC yr−1) and that C accumulation over the last century amounted to 1210 ± 1040 TgC. We attributed this sink to the CO2 fertilization effect on GPP, which led to an increase of 3408 ± 1060 TgC, while both climate and land use reduced the country C stocks by −458 ± 1001 and −1740 ± 878 TgC, respectively. Under different future scenarios, the C sink will likely continue over the 21st century, with decreasing C uptake as the climate forcing becomes more extreme. Our work provides valuable insights on relevant driving processes of the C cycle such as the role of drought in drylands (e.g., grasslands and shrublands) and the impact of climate change on the mean residence time of soil C in tropical ecosystems.