TY - JOUR
T1 - The carbon cycle in Mexico
T2 - Past, present and future of C stocks and fluxes
AU - Murray-Tortarolo, G.
AU - Friedlingstein, P.
AU - Sitch, S.
AU - Jaramillo, V. J.
AU - Murguia-Flores, F.
AU - Anav, A.
AU - Liu, Y.
AU - Arneth, A.
AU - Arvanitis, A.
AU - Harper, A.
AU - Jain, A.
AU - Kato, E.
AU - Koven, C.
AU - Poulter, B.
AU - Stocker, B. D.
AU - Wiltshire, A.
AU - Zaehle, S.
AU - Zeng, N.
N1 - Publisher Copyright:
© 2016 Author(s).
PY - 2016/1/15
Y1 - 2016/1/15
N2 - 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.
AB - 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.
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U2 - 10.5194/bg-13-223-2016
DO - 10.5194/bg-13-223-2016
M3 - Article
AN - SCOPUS:84961348079
SN - 1726-4170
VL - 13
SP - 223
EP - 238
JO - Biogeosciences
JF - Biogeosciences
IS - 1
ER -