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  • 1
    Publication Date: 2013-06-08
    Description: We combine satellite and ground observations during 1950-2011 to study the long-term links between multiple climate (air temperature and cryospheric dynamics) and vegetation (greenness and atmospheric CO2 concentrations) indicators of the growing season of northern ecosystems (〉45oN) and their connection with the carbon cycle. During the last three decades, the thermal potential growing season has lengthened by about 10.5 days ( p 〈 0.01, 1982–2011), which is unprecedented in the context of the past 60 years. The overall lengthening has been stronger and more significant in Eurasia (12.6 days, p 〈 0.01) than North America (6.2 days, p 〉 0.05). The photosynthetic growing season has closely tracked the pace of warming and extension of the potential growing season in spring, but not in autumn when factors such as light and moisture limitation may constrain photosynthesis. The autumnal extension of the photosynthetic growing season since 1982 appears to be about half that of the thermal potential growing season, yielding a smaller lengthening of the photosynthetic growing season (6.7 days at circumpolar scale, p 〈 0.01). Nevertheless, when integrated over the growing season, photosynthetic activity has closely followed the interannual variations and warming trend in cumulative growing season temperatures. This lengthening and intensification of the photosynthetic growing season, manifested principally over Eurasia rather than North America, is associated with a long-term increase (22.2% since 1972, p 〈 0.01) in the amplitude of the CO2 annual cycle at northern latitudes. The springtime extension of the photosynthetic and potential growing seasons has apparently stimulated earlier and stronger net CO2 uptake by northern ecosystems, while the autumnal extension is associated with an earlier net release of CO2 to the atmosphere. These contrasting responses may be critical in determining the impact of continued warming on northern terrestrial ecosystems and the carbon cycle. This article is protected by copyright. All rights reserved.
    Print ISSN: 1354-1013
    Electronic ISSN: 1365-2486
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Published by Wiley
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  • 2
    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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  • 3
    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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  • 4
    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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  • 5
    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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  • 6
    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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  • 7
    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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  • 8
    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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  • 9
    Publication Date: 2013-05-30
    Description: Pronounced increases in winter temperature result in lower seasonal temperature differences, with implications for vegetation seasonality and productivity. Research now indicates that temperature and vegetation seasonality in northern ecosystems have diminished to an extent equivalent to a southerly shift of 4°– 7° in latitude, and may reach the equivalent of up to 20° over the twenty-first century. Nature Climate Change 3 581 doi: 10.1038/nclimate1836
    Print ISSN: 1758-678X
    Electronic ISSN: 1758-6798
    Topics: Geosciences
    Published by Springer Nature
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 386 (1997), S. 698-702 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] We have made use of data from the advanced Very High Resolution Radiometers (AVHRRs) on board the National Oceanic and Atmospheric Administration (NOAA) series of meteorological satellites (NOAA-7, -9 and -11). From daily observations of channel 1 (wavelengths 0.58-0.68 |xm) and channel 2 ...
    Type of Medium: Electronic Resource
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