Climate control of terrestrial carbon exchange across biomes and continents
(2010) In Environmental Research Letters 5(3).- 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... (More)
- 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 (45 degrees N). The sensitivity of NEE to mean annual temperature breaks down at similar to 16 degrees C (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. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/1727349
- author
- organization
- publishing date
- 2010
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- biomes, eddy flux, dryness, temperature, terrestrial carbon sequestration, NEE, climate control, photosynthesis, respiration, global carbon, cycle
- in
- Environmental Research Letters
- volume
- 5
- issue
- 3
- article number
- 034007
- publisher
- IOP Publishing
- external identifiers
-
- wos:000282273700008
- scopus:78049506788
- ISSN
- 1748-9326
- DOI
- 10.1088/1748-9326/5/3/034007
- language
- English
- LU publication?
- yes
- id
- 6cdd39fc-f88d-4d2b-b66c-8a759007f844 (old id 1727349)
- date added to LUP
- 2016-04-01 14:08:25
- date last changed
- 2022-02-19 17:17:11
@article{6cdd39fc-f88d-4d2b-b66c-8a759007f844,
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 (45 degrees N). The sensitivity of NEE to mean annual temperature breaks down at similar to 16 degrees C (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.}},
author = {{Yi, Chuixiang and Ricciuto, Daniel and Li, Runze and Wolbeck, John and Xu, Xiyan and Nilsson, Mats and Aires, Luis and Albertson, John D. and Ammann, Christof and Arain, M. Altaf and de Araujo, Alessandro C. and Aubinet, Marc and Aurela, Mika and Barcza, Zoltan and Barr, Alan and Berbigier, Paul and Beringer, Jason and Bernhofer, Christian and Black, Andrew T. and Bolstad, Paul V. and Bosveld, Fred C. and Broadmeadow, Mark S. J. and Buchmann, Nina and Burns, Sean P. and Cellier, Pierre and Chen, Jingming and Chen, Jiquan and Ciais, Philippe and Clement, Robert and Cook, Bruce D. and Curtis, Peter S. and Dail, D. Bryan and Dellwik, Ebba and Delpierre, Nicolas and Desai, Ankur R. and Dore, Sabina and Dragoni, Danilo and Drake, Bert G. and Dufrene, Eric and Dunn, Allison and Elbers, Jan and Eugster, Werner and Falk, Matthias and Feigenwinter, Christian and Flanagan, Lawrence B. and Foken, Thomas and Frank, John and Fuhrer, Juerg and Gianelle, Damiano and Goldstein, Allen and Goulden, Mike and Granier, Andre and Gruenwald, Thomas and Gu, Lianhong and Guo, Haiqiang and Hammerle, Albin and Han, Shijie and Hanan, Niall P. and Haszpra, Laszlo and Heinesch, Bernard and Helfter, Carole and Hendriks, Dimmie and Hutley, Lindsay B. and Ibrom, Andreas and Jacobs, Cor and Johansson, Torbjörn and Jongen, Marjan and Katul, Gabriel and Kiely, Gerard and Klumpp, Katja and Knohl, Alexander and Kolb, Thomas and Kutsch, Werner L. and Lafleur, Peter and Laurila, Tuomas and Leuning, Ray and Lindroth, Anders and Liu, Heping and Loubet, Benjamin and Manca, Giovanni and Marek, Michal and Margolis, Hank A. and Martin, Timothy A. and Massman, William J. and Matamala, Roser and Matteucci, Giorgio and McCaughey, Harry and Merbold, Lutz and Meyers, Tilden and Migliavacca, Mirco and Miglietta, Franco and Misson, Laurent and Mölder, Meelis and Moncrieff, John and Monson, Russell K. and Montagnani, Leonardo and Montes-Helu, Mario and Moors, Eddy and Moureaux, Christine and Mukelabai, Mukufute M. and Munger, J. William and Myklebust, May and Nagy, Zoltan and Noormets, Asko and Oechel, Walter and Oren, Ram and Pallardy, Stephen G. and Kyaw, Tha Paw U. and Pereira, Joao S. and Pilegaard, Kim and Pinter, Krisztina and Pio, Casimiro and Pita, Gabriel and Powell, Thomas L. and Rambal, Serge and Randerson, James T. and von Randow, Celso and Rebmann, Corinna and Rinne, Janne and Rossi, Federica and Roulet, Nigel and Ryel, Ronald J. and Sagerfors, Jorgen and Saigusa, Nobuko and Sanz, Maria Jose and Mugnozza, Giuseppe-Scarascia and Schmid, Hans Peter and Seufert, Guenther and Siqueira, Mario and Soussana, Jean-Francois and Starr, Gregory and Sutton, Mark A. and Tenhunen, John and Tuba, Zoltan and Tuovinen, Juha-Pekka and Valentini, Riccardo and Vogel, Christoph S. and Wang, Jingxin and Wang, Shaoqiang and Wang, Weiguo and Welp, Lisa R. and Wen, Xuefa and Wharton, Sonia and Wilkinson, Matthew and Williams, Christopher A. and Wohlfahrt, Georg and Yamamoto, Susumu and Yu, Guirui and Zampedri, Roberto and Zhao, Bin and Zhao, Xinquan}},
issn = {{1748-9326}},
keywords = {{biomes; eddy flux; dryness; temperature; terrestrial carbon sequestration; NEE; climate control; photosynthesis; respiration; global carbon; cycle}},
language = {{eng}},
number = {{3}},
publisher = {{IOP Publishing}},
series = {{Environmental Research Letters}},
title = {{Climate control of terrestrial carbon exchange across biomes and continents}},
url = {{http://dx.doi.org/10.1088/1748-9326/5/3/034007}},
doi = {{10.1088/1748-9326/5/3/034007}},
volume = {{5}},
year = {{2010}},
}