http://www.cnr.it/ontology/cnr/individuo/prodotto/ID171077
Climate control of terrestrial carbon exchange across biomes and continents (Articolo in rivista)
- Type
- Label
- Climate control of terrestrial carbon exchange across biomes and continents (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1088/1748-9326/5/3/034007 (literal)
- Alternative label
Chuixiang Yi, Rossi F., et al. Yi C., Ricciuto D., Li R., Wolbeck J., Xu X., Nilsson M., Matteucci G. e altri (2010)
Climate control of terrestrial carbon exchange across biomes and continents
in Environmental research letters
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Chuixiang Yi, Rossi F., et al. Yi C., Ricciuto D., Li R., Wolbeck J., Xu X., Nilsson M., Matteucci G. e altri (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://iopscience.iop.org/1748-9326/5/3/034007 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- Letters 5 (2010) 034007 (10pp) Doi:10.1088/1748-9326/5/3/034007. (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- CNR IBIMET e IBAF (literal)
- Titolo
- Climate control of terrestrial carbon exchange across biomes and continents (literal)
- Abstract
- Understanding the relationships between climate and carbon exchange by terrestrial ecosystems
is critical to predict future levels of atmospheric carbon dioxide because of the potential
accelerating effects of positive climate-carbon cycle feedbacks. However, directly observed
relationships between climate and terrestrial CO2 exchange with the atmosphere across biomes
and continents are lacking. Here we present data describing the relationships between net
ecosystem exchange of carbon (NEE) and climate factors as measured using the eddy
covariance method at 125 unique sites in various ecosystems over six continents with a total of
559 site-years. We find that NEE observed at eddy covariance sites is (1) a strong function of
mean annual temperature at mid- and high-latitudes, (2) a strong function of dryness at mid- and
low-latitudes, and (3) a function of both temperature and dryness around the mid-latitudinal belt
(45oN). The sensitivity of NEE to mean annual temperature breaks down at ~16 oC (a threshold
value of mean annual temperature), above which no further increase of CO2 uptake with
temperature was observed and dryness influence overrules temperature influence. (literal)
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