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  • 1
    Publication Date: 2011-08-27
    Description: Zhao and Running (Reports, 20 August 2010, p. 940) reported a reduction in global terrestrial net primary production (NPP) from 2000 through 2009. We argue that the small trends, regional patterns, and interannual variations that they describe are artifacts of their NPP model. Satellite observations of vegetation activity show no statistically significant changes in more than 85% of the vegetated lands south of 70 degrees N during the same 2000 to 2009 period.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Samanta, Arindam -- Costa, Marcos H -- Nunes, Edson L -- Vieira, Simone A -- Xu, Liang -- Myneni, Ranga B -- New York, N.Y. -- Science. 2011 Aug 26;333(6046):1093; author reply 1093. doi: 10.1126/science.1199048.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geography and Environment, Boston University, Boston, MA 02215, USA. arindam.sam@gmail.com〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21868655" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; Biomass ; *Carbon Cycle ; Carbon Dioxide ; *Droughts ; *Ecosystem ; Photosynthesis ; Plants/*metabolism ; South America
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2003-06-07
    Description: Recent climatic changes have enhanced plant growth in northern mid-latitudes and high latitudes. However, a comprehensive analysis of the impact of global climatic changes on vegetation productivity has not before been expressed in the context of variable limiting factors to plant growth. We present a global investigation of vegetation responses to climatic changes by analyzing 18 years (1982 to 1999) of both climatic data and satellite observations of vegetation activity. Our results indicate that global changes in climate have eased several critical climatic constraints to plant growth, such that net primary production increased 6% (3.4 petagrams of carbon over 18 years) globally. The largest increase was in tropical ecosystems. Amazon rain forests accounted for 42% of the global increase in net primary production, owing mainly to decreased cloud cover and the resulting increase in solar radiation.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Nemani, Ramakrishna R -- Keeling, Charles D -- Hashimoto, Hirofumi -- Jolly, William M -- Piper, Stephen C -- Tucker, Compton J -- Myneni, Ranga B -- Running, Steven W -- New York, N.Y. -- Science. 2003 Jun 6;300(5625):1560-3.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Forestry, University of Montana, Missoula, MT 59801, USA. nemani@ntsg.umt.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/12791990" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; Carbon/analysis ; Carbon Dioxide ; *Climate ; *Ecosystem ; Geography ; *Plant Development ; Rain ; Seasons ; Soil ; Sunlight ; Temperature ; Time Factors ; Tropical Climate ; Volcanic Eruptions
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2002-06-01
    Description: A biogeochemical model of vegetation using observed climate data predicts the high northern latitude greening trend over the past two decades observed by satellites and a marked setback in this trend after the Mount Pinatubo volcano eruption in 1991. The observed trend toward earlier spring budburst and increased maximum leaf area is produced by the model as a consequence of biogeochemical vegetation responses mainly to changes in temperature. The post-Pinatubo decline in vegetation in 1992-1993 is apparent as the effect of temporary cooling caused by the eruption. High-latitude CO(2) uptake during these years is predicted as a consequence of the differential response of heterotrophic respiration and net primary production.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lucht, Wolfgang -- Prentice, I Colin -- Myneni, Ranga B -- Sitch, Stephen -- Friedlingstein, Pierre -- Cramer, Wolfgang -- Bousquet, Philippe -- Buermann, Wolfgang -- Smith, Benjamin -- New York, N.Y. -- Science. 2002 May 31;296(5573):1687-9.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Potsdam Institute for Climate Impact Research, Post Office Box 601203, D-14412 Potsdam, Germany. Wolfgang.Lucht@pik-potsdam.de〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/12040194" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; Biomass ; Carbon Dioxide/metabolism ; *Climate ; Computer Simulation ; *Ecosystem ; Geography ; Models, Biological ; *Plant Development ; Plant Leaves/*growth & development ; Seasons ; Temperature ; *Volcanic Eruptions
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2014-05-23
    Description: The land and ocean act as a sink for fossil-fuel emissions, thereby slowing the rise of atmospheric carbon dioxide concentrations. Although the uptake of carbon by oceanic and terrestrial processes has kept pace with accelerating carbon dioxide emissions until now, atmospheric carbon dioxide concentrations exhibit a large variability on interannual timescales, considered to be driven primarily by terrestrial ecosystem processes dominated by tropical rainforests. We use a terrestrial biogeochemical model, atmospheric carbon dioxide inversion and global carbon budget accounting methods to investigate the evolution of the terrestrial carbon sink over the past 30 years, with a focus on the underlying mechanisms responsible for the exceptionally large land carbon sink reported in 2011 (ref. 2). Here we show that our three terrestrial carbon sink estimates are in good agreement and support the finding of a 2011 record land carbon sink. Surprisingly, we find that the global carbon sink anomaly was driven by growth of semi-arid vegetation in the Southern Hemisphere, with almost 60 per cent of carbon uptake attributed to Australian ecosystems, where prevalent La Nina conditions caused up to six consecutive seasons of increased precipitation. In addition, since 1981, a six per cent expansion of vegetation cover over Australia was associated with a fourfold increase in the sensitivity of continental net carbon uptake to precipitation. Our findings suggest that the higher turnover rates of carbon pools in semi-arid biomes are an increasingly important driver of global carbon cycle inter-annual variability and that tropical rainforests may become less relevant drivers in the future. More research is needed to identify to what extent the carbon stocks accumulated during wet years are vulnerable to rapid decomposition or loss through fire in subsequent years.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Poulter, Benjamin -- Frank, David -- Ciais, Philippe -- Myneni, Ranga B -- Andela, Niels -- Bi, Jian -- Broquet, Gregoire -- Canadell, Josep G -- Chevallier, Frederic -- Liu, Yi Y -- Running, Steven W -- Sitch, Stephen -- van der Werf, Guido R -- England -- Nature. 2014 May 29;509(7502):600-3. doi: 10.1038/nature13376. Epub 2014 May 21.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Montana State University, Institute on Ecosystems and the Department of Ecology, Bozeman, Montana 59717, USA [2] Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA CNRS UVSQ, 91191 Gif Sur Yvette, France. ; 1] Swiss Federal Research Institute WSL, Dendroclimatology, Zurcherstrasse 111, Birmensdorf 8903, Switzerland [2] Oeschger Centre for Climate Change Research, University of Bern, CH-3012 Bern, Switzerland. ; Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA CNRS UVSQ, 91191 Gif Sur Yvette, France. ; Department of Earth and Environment, Boston University, 685 Commonwealth Avenue, Boston, Massachusetts 02215, USA. ; Faculty of Earth and Life Sciences, VU University Amsterdam, 1085 De Boelelaan, 1081HV, Amsterdam, The Netherlands. ; Global Carbon Project, CSIRO, Marine and Atmospheric Research, Canberra, Australian Capital Territory 2601, Australia. ; ARC Centre of Excellence for Climate Systems Science & Climate Change Research Centre, University of New South Wales, Sydney, New South Wales 2052, Australia. ; Department of Ecosystem and Conservation Sciences, University of Montana, Missoula, Montana 59812, USA. ; College of Engineering, Computing and Mathematics, University of Exeter, Exeter EX4 4QF, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24847888" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Australia ; Carbon Dioxide/analysis ; *Carbon Sequestration ; *Desert Climate ; *Ecosystem ; El Nino-Southern Oscillation ; Fires ; Models, Theoretical ; Rain ; Seasons ; Uncertainty
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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