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

丰满有漂亮

Carbon Cycles in Forests,ound to be influenced by soil physical properties, soil biota, length of the frost season, and hydrothermal conditions. According to long-term eddy-correlation data, the annual NEE in medium-productivity larch forest was 212 ± 34 g C m. year., that in high-productivity larch forest was 243 ± 23 g C 

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Water-Carbon Cycle in Dendrochronology,hniques to the investigation of the water and carbon cycles that are characteristic of these forest ecosystems. I also discuss limitations presented by the use of dendrochronological techniques in studying forest ecosystem carbon cycling and future goals in overcoming these limitations.

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Permafrost-Forest Dynamics,the active layer and upper part of the permafrost during recent decades. An increase in the mean active-layer depth of only a few tens of centimetres would release large amounts of water and carbon. Predicting permafrost landscape changes is not straightforward; it is hindered by uncertainty, by the

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Remote Sensing of Vegetation,und biomass, PFT, and growing season duration in eastern Siberia. We then introduce our own studies, which compared in situ field observations with satellite observations, and examine the usability and prospects of remote-sensing techniques, including uncertainties and other related issues, for obse