GRL dataset
Description
Lakes and reservoirs are significant sources of methane (CH4) and carbon dioxide (CO2) in global scale, yet their responses to climate change remain inadequately studied.We present high-resolution vertical profiles of CH4 and CO2 concentrations to elucidate their production, storage, and emission dynamics in a eutrophic subtropical reservoir. Methanogenesis initiated in the hypoxic hypolimnion led to a steady rise in CH4 and CO2 levels, with CH4 comprising up to ~50% of total carbonaceous greenhouse gases during ventilation. During stratification, oxic CH4 production dominated in surface waters, while vertical mixing, driven by cooling and wind events, enhanced hypolimnetic CH4 release. A synthesis of global CH4 fluxes and stratification days suggests that prolonged stratification may enhance CH4 storage but limit its release from bottom waters. With increasing eutrophication and global warming, enhanced stratification could amplify the climatic impact of aerobic, rather than anaerobic, CH4 production in subtropical lakes and reservoirs.
Files
Steps to reproduce
Our dataset include consisting of hydrological parameters (water temperature and dissolved oxygen) and greenhouse gas concentrations (CH4 and CO2) for a subtropical reservoir in monthly layers of one metre for a period of two years, as well as global diffusive emission fluxes of CH4 and CO2 and stratification duration.
Institutions
- Xiamen UniversityFujian, Xiamen
Categories
Funders
- National Natural Science Foundation of ChinaBeijing, China
- Innovation Fund for Scientific and Technological Personnel of Hainan Province
- Collaborative Innovation Center of Marine Science and Technology in Hainan University