Role of methane and biogenic volatile organic compound sources in late glacial and Holocene fluctuations of atmospheric methane concentrations
about
Elevated atmospheric CO2 concentration leads to increased whole-plant isoprene emission in hybrid aspen (Populus tremula × Populus tremuloides).Isotopic evidence of multiple controls on atmospheric oxidants over climate transitions.Understanding the glacial methane cycle.Global emissions of terpenoid VOCs from terrestrial vegetation in the last millennium.Onset of photosynthesis in spring speeds up monoterpene synthesis and leads to emission bursts.Contrasting wetland CH4 emission responses to simulated glacial atmospheric CO2 in temperate bogs and fens.Early anthropogenic CH4emissions and the variation of CH4and13CH4over the last millenniumThe shift in plant species composition in a subarctic mountain birch forest floor due to climate change would modify the biogenic volatile organic compound emission profileNon-methane biogenic volatile organic compound emissions from boreal peatland microcosms under warming and water table drawdownGlacial-interglacial water cycle, global monsoon and atmospheric methane changesGlacial wetland distribution and methane emissions estimated from PMIP2 climate simulationsReconciling the changes in atmospheric methane sources and sinks between the Last Glacial Maximum and the pre-industrial eraSystematic biases in large-scale estimates of wetland methane emissions arising from water table formulationsIndependent variations of CH4 emissions and isotopic composition over the past 160,000 yearsReduction of the temperature sensitivity of minerotrophic fen methane emissions by simulated glacial atmospheric carbon dioxide starvationNon-methane volatile organic compound flux from a subarctic mire in Northern SwedenIn search of an ice core signal to differentiate between source-driven and sink-driven changes in atmospheric methaneHolocene radiative forcing impact of northern peatland carbon accumulation and methane emissionsFlooding of the continental shelves as a contributor to deglacial CH4riseControls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial periodThe role of atomic chlorine in glacial-interglacial changes in the carbon-13 content of atmospheric methane
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P2860
Role of methane and biogenic volatile organic compound sources in late glacial and Holocene fluctuations of atmospheric methane concentrations
description
article
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wetenschappelijk artikel
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наукова стаття, опублікована в червні 2006
@uk
name
Role of methane and biogenic v ...... spheric methane concentrations
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Role of methane and biogenic v ...... spheric methane concentrations
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type
label
Role of methane and biogenic v ...... spheric methane concentrations
@en
Role of methane and biogenic v ...... spheric methane concentrations
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prefLabel
Role of methane and biogenic v ...... spheric methane concentrations
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Role of methane and biogenic v ...... spheric methane concentrations
@nl
P2860
P356
P1476
Role of methane and biogenic v ...... spheric methane concentrations
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P2093
Didier A. Hauglustaine
P2860
P356
10.1029/2005GB002590
P577
2006-06-01T00:00:00Z