Your browser doesn't support javascript.
loading
Recent increases in terrestrial carbon uptake at little cost to the water cycle.
Cheng, Lei; Zhang, Lu; Wang, Ying-Ping; Canadell, Josep G; Chiew, Francis H S; Beringer, Jason; Li, Longhui; Miralles, Diego G; Piao, Shilong; Zhang, Yongqiang.
Afiliación
  • Cheng L; CSIRO Land and Water, Black Mountain, Canberra, ACT, 2601, Australia. Lu.Zhang@CSIRO.au.
  • Zhang L; CSIRO Land and Water, Black Mountain, Canberra, ACT, 2601, Australia.
  • Wang YP; CSIRO Oceans and Atmosphere, PMB #1, Aspendale, VIC, 3195, Australia.
  • Canadell JG; Global Carbon Project, CSIRO Oceans and Atmosphere, GPO Box 3023, Canberra, ACT, 2601, Australia.
  • Chiew FHS; CSIRO Land and Water, Black Mountain, Canberra, ACT, 2601, Australia.
  • Beringer J; School of Agriculture and Environment, The University of Western Australia, Perth, WA, 6009, Australia.
  • Li L; School of Life Sciences, University of Technology Sydney, Ultimo, NSW, 2007, Australia.
  • Miralles DG; Laboratory of Hydrology and Water Management, Ghent University, Ghent, 9000, Belgium.
  • Piao S; Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, 100871, China.
  • Zhang Y; Key Laboratory of Alpine Ecology and Biodiversity, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China.
Nat Commun ; 8(1): 110, 2017 07 24.
Article en En | MEDLINE | ID: mdl-28740122
ABSTRACT
Quantifying the responses of the coupled carbon and water cycles to current global warming and rising atmospheric CO2 concentration is crucial for predicting and adapting to climate changes. Here we show that terrestrial carbon uptake (i.e. gross primary production) increased significantly from 1982 to 2011 using a combination of ground-based and remotely sensed land and atmospheric observations. Importantly, we find that the terrestrial carbon uptake increase is not accompanied by a proportional increase in water use (i.e. evapotranspiration) but is largely (about 90%) driven by increased carbon uptake per unit of water use, i.e. water use efficiency. The increased water use efficiency is positively related to rising CO2 concentration and increased canopy leaf area index, and negatively influenced by increased vapour pressure deficits. Our findings suggest that rising atmospheric CO2 concentration has caused a shift in terrestrial water economics of carbon uptake.The response of the coupled carbon and water cycles to anthropogenic climate change is unclear. Here, the authors show that terrestrial carbon uptake increased significantly from 1982 to 2011 and that this increase is largely driven by increased water-use efficiency, rather than an increase in water use.

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Tipo de estudio: Health_economic_evaluation / Prognostic_studies Idioma: En Revista: Nat Commun Asunto de la revista: BIOLOGIA / CIENCIA Año: 2017 Tipo del documento: Article País de afiliación: Australia

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Tipo de estudio: Health_economic_evaluation / Prognostic_studies Idioma: En Revista: Nat Commun Asunto de la revista: BIOLOGIA / CIENCIA Año: 2017 Tipo del documento: Article País de afiliación: Australia