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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. Murguia-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
  • University of Exeter
  • Instituto de Investigaciones en Ecosistemas y Sustentabilidad
  • University of Bristol
  • University of New South Wales
  • Institute of Meteorology and Climate Research
  • University of Illinois at Urbana-Champaign
  • Institute of Applied Energy (IAE)
  • Ernest Orlando Lawrence Berkeley National Laboratory
  • Montana State University
  • Imperial College London
  • Now at Met Office Hadley Centre
  • Max Planck Institute for Biogeochemistry
  • University of Maryland

Research output: Contribution to journalArticlepeer-review

Abstract

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 TgCyr-1 and a total C stock of 34506 ± 7483 TgC, with 20347 ± 4622TgC in vegetation and 14159 ± 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 TgCyr-1) and that C accumulation over the last century amounted to 1210 ± 1040TgC. We attributed this sink to the CO2 fertilization effect on GPP, which led to an increase of 3408 ± 1060TgC, while both climate and land use reduced the country C stocks by-458 ± 1001 and-1740 ± 878TgC, 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.

Original languageEnglish
Pages (from-to)223-238
Number of pages16
JournalBiogeosciences
Volume13
Issue number1
DOIs
Publication statusPublished - 15 Jan 2016
Externally publishedYes

UN SDGs

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

  1. SDG 13 - Climate Action
    SDG 13 Climate Action
  2. SDG 15 - Life on Land
    SDG 15 Life on Land

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