Titlebook: Water-Carbon Dynamics in Eastern Siberia; Takeshi Ohta,Tetsuya Hiyama,Trofim C. Maximov Book 2019 Springer Nature Singapore Pte Ltd. 2019

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Methane and Biogenic Volatile Organic Compound Emissions in Eastern Siberia,ces of CH. can be distinguished: ecosystem CH. (produced from recently photosynthesized carbon in wetlands), old-carbon CH. (generated by mobilization of old soil carbon), and deep CH. (liberated from shallow gas reservoirs in the permafrost, including hydrates). The data uncertainty of these source

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Stable Isotopes of Water in Permafrost Ecosystem, of water have been widely used in studies of the water cycle because summer precipitation, winter snowfall, and ground ice can be isotopically discerned. In early summer, larch trees use soil water derived from winter snowfall; if the summer is wet, soil water from summer rainfall is subsequently u

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Stable Isotopes of Water in Permafrost Ecosystem, of water have been widely used in studies of the water cycle because summer precipitation, winter snowfall, and ground ice can be isotopically discerned. In early summer, larch trees use soil water derived from winter snowfall; if the summer is wet, soil water from summer rainfall is subsequently u

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Water-Carbon Cycle in Dendrochronology,and carbon cycling. This method is a powerful tool to extend the short-term record of water and carbon cycling in the decades preceding data monitoring. Traditionally, tree-ring width and density proxies have been used for this purpose; however, analysis methods for the examination of stable isotope

mendacity

Water-Carbon Cycle in Dendrochronology,and carbon cycling. This method is a powerful tool to extend the short-term record of water and carbon cycling in the decades preceding data monitoring. Traditionally, tree-ring width and density proxies have been used for this purpose; however, analysis methods for the examination of stable isotope

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Permafrost-Forest Dynamics,erous boreal (taiga) forest. Underlying the boreal ecosystem is an extensive and massive ice layer within the permafrost (Yedoma), which was crucial for the development of large ground subsidence during the Holocene, which is closely related to ice volume loss. Therefore, scattered large grassland d

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