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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: 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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  • 3
    Publication Date: 2014-04-25
    Description: Tropical forests are global epicentres of biodiversity and important modulators of climate change, and are mainly constrained by rainfall patterns. The severe short-term droughts that occurred recently in Amazonia have drawn attention to the vulnerability of tropical forests to climatic disturbances. The central African rainforests, the second-largest on Earth, have experienced a long-term drying trend whose impacts on vegetation dynamics remain mostly unknown because in situ observations are very limited. The Congolese forest, with its drier conditions and higher percentage of semi-evergreen trees, may be more tolerant to short-term rainfall reduction than are wetter tropical forests, but for a long-term drought there may be critical thresholds of water availability below which higher-biomass, closed-canopy forests transition to more open, lower-biomass forests. Here we present observational evidence for a widespread decline in forest greenness over the past decade based on analyses of satellite data (optical, thermal, microwave and gravity) from several independent sensors over the Congo basin. This decline in vegetation greenness, particularly in the northern Congolese forest, is generally consistent with decreases in rainfall, terrestrial water storage, water content in aboveground woody and leaf biomass, and the canopy backscatter anomaly caused by changes in structure and moisture in upper forest layers. It is also consistent with increases in photosynthetically active radiation and land surface temperature. These multiple lines of evidence indicate that this large-scale vegetation browning, or loss of photosynthetic capacity, may be partially attributable to the long-term drying trend. Our results suggest that a continued gradual decline of photosynthetic capacity and moisture content driven by the persistent drying trend could alter the composition and structure of the Congolese forest to favour the spread of drought-tolerant species.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Zhou, Liming -- Tian, Yuhong -- Myneni, Ranga B -- Ciais, Philippe -- Saatchi, Sassan -- Liu, Yi Y -- Piao, Shilong -- Chen, Haishan -- Vermote, Eric F -- Song, Conghe -- Hwang, Taehee -- England -- Nature. 2014 May 1;509(7498):86-90. doi: 10.1038/nature13265. Epub 2014 Apr 23.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York (SUNY), Albany, New York 12222, USA. ; I. M. Systems Group (IMSG), National Oceanic and Atmospheric Administration/National Environmental Satellite, Data, and Information Service/The Center for Satellite Applications and Research (NOAA/NESDIS/STAR), 5830 University Research Court, College Park, Maryland 20740, USA. ; Department of Earth and Environment, Boston University, Boston, Massachusetts 02215, USA. ; Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA-CNRS-UVSQ, 91191 Gif sur Yvette Cedex, France. ; Jet Propulsion Laboratory, Pasadena, California 91109, USA. ; 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 Ecology, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China. ; Key Laboratory of Meteorological Disaster, Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044, China. ; NASA Goddard Space Flight Center, Code 619, Greenbelt, Maryland 20771, USA. ; 1] Department of Geography, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 29599, USA [2] School of Forestry and Landscape Architecture, Anhui Agricultural University, Hefei, Anhui 230036, China. ; Institute for the Environment, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 29599, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24759324" target="_blank"〉PubMed〈/a〉
    Keywords: Acclimatization ; Biodiversity ; Biomass ; Chlorophyll/analysis/metabolism ; Climate Change/*statistics & numerical data ; Congo ; Droughts/statistics & numerical data ; Photosynthesis ; Plant Leaves/*growth & development/metabolism ; *Rain ; Satellite Imagery ; Seasons ; Temperature ; Time Factors ; Trees/*growth & development/metabolism ; *Tropical Climate ; Water/analysis/metabolism ; Wood/growth & development/metabolism
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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