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How drought events during the last century have impacted biomass carbon in Amazonian rainforests

During the last two decades, inventory data show that droughts have reduced biomass carbon sink of the Amazon forest by causing mortality to exceed growth. However, process‐based models have struggled to include drought‐induced responses of growth and mortality and have not been evaluated against pl...

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Detalles Bibliográficos
Autores principales: Yao, Yitong, Ciais, Philippe, Viovy, Nicolas, Joetzjer, Emilie, Chave, Jerome
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10100251/
https://www.ncbi.nlm.nih.gov/pubmed/36285645
http://dx.doi.org/10.1111/gcb.16504
Descripción
Sumario:During the last two decades, inventory data show that droughts have reduced biomass carbon sink of the Amazon forest by causing mortality to exceed growth. However, process‐based models have struggled to include drought‐induced responses of growth and mortality and have not been evaluated against plot data. A process‐based model, ORCHIDEE‐CAN‐NHA, including forest demography with tree cohorts, plant hydraulic architecture and drought‐induced tree mortality, was applied over Amazonia rainforests forced by gridded climate fields and rising CO(2) from 1901 to 2019. The model reproduced the decelerating signal of net carbon sink and drought sensitivity of aboveground biomass (AGB) growth and mortality observed at forest plots across selected Amazon intact forests for 2005 and 2010. We predicted a larger mortality rate and a more negative sensitivity of the net carbon sink during the 2015/16 El Niño compared with the former droughts. 2015/16 was indeed the most severe drought since 1901 regarding both AGB loss and area experiencing a severe carbon loss. We found that even if climate change did increase mortality, elevated CO(2) contributed to balance the biomass mortality, since CO(2)‐induced stomatal closure reduces transpiration, thus, offsets increased transpiration from CO(2)‐induced higher foliage area.