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  • 1
    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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  • 2
    Publication Date: 2013-09-06
    Description: Temperature data over the past five decades show faster warming of the global land surface during the night than during the day. This asymmetric warming is expected to affect carbon assimilation and consumption in plants, because photosynthesis in most plants occurs during daytime and is more sensitive to the maximum daily temperature, Tmax, whereas plant respiration occurs throughout the day and is therefore influenced by both Tmax and the minimum daily temperature, Tmin. Most studies of the response of terrestrial ecosystems to climate warming, however, ignore this asymmetric forcing effect on vegetation growth and carbon dioxide (CO2) fluxes. Here we analyse the interannual covariations of the satellite-derived normalized difference vegetation index (NDVI, an indicator of vegetation greenness) with Tmax and Tmin over the Northern Hemisphere. After removing the correlation between Tmax and Tmin, we find that the partial correlation between Tmax and NDVI is positive in most wet and cool ecosystems over boreal regions, but negative in dry temperate regions. In contrast, the partial correlation between Tmin and NDVI is negative in boreal regions, and exhibits a more complex behaviour in dry temperate regions. We detect similar patterns in terrestrial net CO2 exchange maps obtained from a global atmospheric inversion model. Additional analysis of the long-term atmospheric CO2 concentration record of the station Point Barrow in Alaska suggests that the peak-to-peak amplitude of CO2 increased by 23 +/- 11% for a +1 degrees C anomaly in Tmax from May to September over lands north of 51 degrees N, but decreased by 28 +/- 14% for a +1 degrees C anomaly in Tmin. These lines of evidence suggest that asymmetric diurnal warming, a process that is currently not taken into account in many global carbon cycle models, leads to a divergent response of Northern Hemisphere vegetation growth and carbon sequestration to rising temperatures.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Peng, Shushi -- Piao, Shilong -- Ciais, Philippe -- Myneni, Ranga B -- Chen, Anping -- Chevallier, Frederic -- Dolman, Albertus J -- Janssens, Ivan A -- Penuelas, Josep -- Zhang, Gengxin -- Vicca, Sara -- Wan, Shiqiang -- Wang, Shiping -- Zeng, Hui -- England -- Nature. 2013 Sep 5;501(7465):88-92. doi: 10.1038/nature12434.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24005415" target="_blank"〉PubMed〈/a〉
    Keywords: Carbon/metabolism ; Carbon Cycle ; Carbon Dioxide/metabolism ; Cell Respiration ; Circadian Rhythm ; *Darkness ; Ecosystem ; *Geography ; *Global Warming ; Photosynthesis/radiation effects ; Plants/*metabolism/radiation effects ; Sunlight ; Temperature
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2014-01-28
    Description: Earth system models project that the tropical land carbon sink will decrease in size in response to an increase in warming and drought during this century, probably causing a positive climate feedback. But available data are too limited at present to test the predicted changes in the tropical carbon balance in response to climate change. Long-term atmospheric carbon dioxide data provide a global record that integrates the interannual variability of the global carbon balance. Multiple lines of evidence demonstrate that most of this variability originates in the terrestrial biosphere. In particular, the year-to-year variations in the atmospheric carbon dioxide growth rate (CGR) are thought to be the result of fluctuations in the carbon fluxes of tropical land areas. Recently, the response of CGR to tropical climate interannual variability was used to put a constraint on the sensitivity of tropical land carbon to climate change. Here we use the long-term CGR record from Mauna Loa and the South Pole to show that the sensitivity of CGR to tropical temperature interannual variability has increased by a factor of 1.9 +/- 0.3 in the past five decades. We find that this sensitivity was greater when tropical land regions experienced drier conditions. This suggests that the sensitivity of CGR to interannual temperature variations is regulated by moisture conditions, even though the direct correlation between CGR and tropical precipitation is weak. We also find that present terrestrial carbon cycle models do not capture the observed enhancement in CGR sensitivity in the past five decades. More realistic model predictions of future carbon cycle and climate feedbacks require a better understanding of the processes driving the response of tropical ecosystems to drought and warming.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Wang, Xuhui -- Piao, Shilong -- Ciais, Philippe -- Friedlingstein, Pierre -- Myneni, Ranga B -- Cox, Peter -- Heimann, Martin -- Miller, John -- Peng, Shushi -- Wang, Tao -- Yang, Hui -- Chen, Anping -- England -- Nature. 2014 Feb 13;506(7487):212-5. doi: 10.1038/nature12915. Epub 2014 Jan 26.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China. ; 1] Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China [2] Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China. ; 1] Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China [2] Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, 91191 Gif-sur-Yvette, France. ; College of Engineering, Mathematics, and Physical Sciences, University of Exeter, Exeter EX4 4QF, UK. ; Department of Earth and Environment, Boston University, Boston, Massachusetts 02215, USA. ; Max Planck Institute for Biogeochemistry, 07701 Jena, Germany. ; 1] Global Monitoring Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, Colorado 80305, USA [2] Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, USA. ; Department of Ecology and Evolutionary Biology, Princeton University, Princeton, New Jersey 08544-1003, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24463514" target="_blank"〉PubMed〈/a〉
    Keywords: Antarctic Regions ; Atmosphere/chemistry ; Carbon/analysis/metabolism ; Carbon Cycle/*physiology ; Carbon Dioxide/metabolism ; Carbon Sequestration ; Droughts ; Ecosystem ; Global Warming ; Hawaii ; History, 20th Century ; History, 21st Century ; Humidity ; Models, Theoretical ; Rain ; *Temperature ; *Tropical Climate
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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