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Temporal and spatial variations in CH4 concentrations in a Japanese warm-temperate mixed forest

机译:日本温带混交林中CH4浓度的时空变化

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摘要

To clarify the characteristics of the variation in methane (CH4) concentrations in a warm-temperate mixed forest in Japan, we measured vertical profiles and daily and seasonal variations in CH4 concentrations, and soil and foliage (Quercus serrata) CH_4 fluxes. CH4 concentrations increased during rainy periods, and decreased in August. Almost constant CH4 uptake was observed at the forest floor throughout the year, but no CH4 flux was observed from the foliage. In the profile measurements, the CH4 concentration was slightly higher at canopy height when friction velocity (u*) was lower than 0.3 m s~(-1). These phenomena were observed on the same day at micrometeorological towers in ridge and valley positions. Variations in CH4 concentrations increased in summer, around ground level, and at canopy height. These results suggest that certain large scale factors govern variations in CH4 concentration around ground level and at canopy height. To understand the overall role of the forest in CH4 circulation, more continuous measurements as close as possible to sinks and sources will be needed.
机译:为了弄清日本温带混交林中甲烷(CH4)浓度变化的特征,我们测量了垂直剖面以及CH4浓度,土壤和枝叶(Quercus serrata)CH_4通量的每日和季节性变化。 CH4浓度在雨季增加,而在8月减少。全年在森林地层观察到几乎恒定的CH4吸收量,但从树叶中未观察到CH4通量。在剖面测量中,当摩擦速度(u *)低于0.3 m s〜(-1)时,冠层高度的CH4浓度略高。这些现象是在同一天在山脊和山谷位置的微气象塔上观察到的。 CH4浓度的变化在夏季,地面附近和树冠高度处增加。这些结果表明,某些大规模因素控制着地面附近和冠层高度CH4浓度的变化。为了了解森林在CH4循环中的总体作用,需要进行更连续的测量,并尽可能靠近汇和源。

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