Abstract
Methane (CH4) is one of the three most important greenhouse gases. To date, observations of ecosystem-scale methane (CH4) fluxes in forests are currently lacking in the global CH4 budget. The environmental factors controlling CH4 flux dynamics remain poorly understood at the ecosystem scale. In this study, we used a state-of-the-art eddy covariance technique to continuously measure the CH4 flux from 2016 to 2018 in a subtropical forest of Zhejiang Province in China, quantify the annual CH4 budget and investigate its control factors. We found that the total annual CH4 budget was 1.15 ± 0.28~4.79 ± 0.49 g CH4 m−2 year−1 for 2017–2018. The daily CH4 flux reached an emission peak of 0.145 g m−2 d−1 during winter and an uptake peak of −0.142 g m−2 d−1 in summer. During the whole study period, the studied forest region acted as a CH4 source (78.65%) during winter and a sink (21.35%) in summer. Soil temperature had a negative relationship (p < 0.01; R2 = 0.344) with CH4 flux but had a positive relationship with soil moisture (p < 0.01; R2 = 0.348). Our results showed that soil temperature and moisture were the most important factors controlling the ecosystem-scale CH4 flux dynamics of subtropical forests in the Tianmu Mountain Nature Reserve in Zhejiang Province, China. Subtropical forest ecosystems in China acted as a net source of methane emissions from 2016 to 2018, providing positive feedback to global climate warming.
Highlights
Methane (CH4) is an important greenhouse gas and accounts for approximately 32% of the global radiative forcing
Major CH4 sources have been identified [4], we still lack a complete understanding of ecosystem-specific information on CH4 sinks and sources that could be significant factors contributing to global variations in CH4 sinks and sources [2,5,6]
Daily soil moisture decreased from June and reached the lowest value of 19.5% in August 2016
Summary
Methane (CH4) is an important greenhouse gas and accounts for approximately 32% of the global radiative forcing. It has 28–32 times higher global warming potential over a 100-year time horizon than does carbon dioxide (CO2) [1,2]. Subtropical forests, as an important part of forest ecosystems, are rich in tree species, characterized by complex stand structures and various environmental conditions [10,11,12], and they play an important role in the global greenhouse gas budget [2,5,11]. It is important to understand CH4 sinks and sources in subtropical forest ecosystems and CH4 exchange between the atmosphere and forests
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