Publication | Open Access
Global methane and nitrous oxide emissions from inland waters and estuaries
153
Citations
41
References
2022
Year
Inland waters (rivers, reservoirs, lakes, ponds, streams) and estuaries are significant emitters of methane (CH<sub>4</sub> ) and nitrous oxide (N<sub>2</sub> O) to the atmosphere, while global estimates of these emissions have been hampered due to the lack of a worldwide comprehensive data set of CH<sub>4</sub> and N<sub>2</sub> O flux components. Here, we synthesize 2997 in-situ flux or concentration measurements of CH<sub>4</sub> and N<sub>2</sub> O from 277 peer-reviewed publications to estimate global CH<sub>4</sub> and N<sub>2</sub> O emissions from inland waters and estuaries. Inland waters including rivers, reservoirs, lakes, and streams together release 95.18 Tg CH<sub>4</sub> year<sup>-1</sup> (ebullition plus diffusion) and 1.48 Tg N<sub>2</sub> O year<sup>-1</sup> (diffusion) to the atmosphere, yielding an overall CO<sub>2</sub> -equivalent emission total of 3.06 Pg CO<sub>2</sub> year<sup>-1</sup> . The estimate of CH<sub>4</sub> and N<sub>2</sub> O emissions represents roughly 60% of CO<sub>2</sub> emissions (5.13 Pg CO<sub>2</sub> year<sup>-1</sup> ) from these four inland aquatic systems, among which lakes act as the largest emitter for both CH<sub>4</sub> and N<sub>2</sub> O. Ebullition showed as a dominant flux component of CH<sub>4</sub> , contributing up to 62%-84% of total CH<sub>4</sub> fluxes across all inland waters. Chamber-derived CH<sub>4</sub> emission rates are significantly greater than those determined by diffusion model-based methods for commonly capturing of both diffusive and ebullitive fluxes. Water dissolved oxygen (DO) showed as a dominant factor among all variables to influence both CH<sub>4</sub> (diffusive and ebullitive) and N<sub>2</sub> O fluxes from inland waters. Our study reveals a major oversight in regional and global CH<sub>4</sub> budgets from inland waters, caused by neglecting the dominant role of ebullition pathways in those emissions. The estimated indirect N<sub>2</sub> O EF<sub>5</sub> values suggest that a downward refinement is required in current IPCC default EF<sub>5</sub> values for inland waters and estuaries. Our findings further indicate that a comprehensive understanding of the magnitude and patterns of CH<sub>4</sub> and N<sub>2</sub> O emissions from inland waters and estuaries is essential in defining the way of how these aquatic systems will shape our climate.
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