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      Carbon Emissions From Chinese Inland Waters: Current Progress and Future Challenges

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          Abstract

          Inland waters are significant emitters of greenhouse gases for the atmosphere and play an important role in the global carbon cycle. With a vast land area in East Asia spanning a broad range of climatic conditions, China has a large number of natural and human‐made water bodies. These inland water systems are of global importance because of their high carbon emission fluxes. Over the past decades, China has experienced unprecedented environmental changes driven by rapid economic development, which have profoundly modified its inland water carbon biogeochemistry and associated emissions. This review focuses on carbon dioxide (CO 2) and methane (CH 4) emission dynamics from China's inland waters in response to global change. Major drivers of CO 2 and CH 4 emissions, including aquatic metabolism, hydrological and climatic factors, and prevailing human impacts, are examined. To advance our understanding of carbon emissions from China's inland waters, we further identify several critical knowledge gaps, such as inadequate research in headwater streams and the climate‐sensitive Tibetan Plateau aquatic ecosystems. Furthermore, insufficient understanding of carbon emissions from inland waters undergoing extensive human interventions (e.g., damming, flow regulation, pollution, and farming practices in aquaculture ponds) is highlighted. We suggest that future efforts should be made to better capture the spatiotemporal heterogeneity in dissolved CO 2 and CH 4 concentrations and fluxes across China as well as their long‐term trends. To overcome uncertainties in carbon sources and current flux estimates, future research to mechanistically understand carbon transport and transformation in Chinese inland waters and their underlying processes is particularly needed.

          Plain Language Summary

          Inland waters (e.g., streams, rivers, lakes, reservoirs, and ponds) are important sources of greenhouse gases (i.e., CO 2 and CH 4) for the atmosphere, affecting the earth's carbon balance. With a vast land area (∼9.6 million km 2) and diverse climate regions, China contains numerous natural and man‐made water bodies. Dissolved carbon dioxide (CO 2) and methane (CH 4) emissions from these inland water systems have been significantly disturbed by global climate change and human activities. This review focuses on the current research progress of CO 2 and CH 4 emissions from China's inland waters. Major factors controlling dissolved CO 2 and CH 4 emission dynamics are examined. Furthermore, we discuss the shortcomings of current research on inland water carbon emissions in climate‐sensitive regions and anthropogenically disturbed regions of China. There is a pressing need to strengthen the monitoring of aquatic CO 2 and CH 4 emissions over space and time and to gain a deeper understanding of the underlying mechanisms.

          Key Points

          • Chinese inland waters have significantly higher water‐to‐air carbon emission fluxes than lateral transport of carbon to the coastal ocean

          • Aquatic metabolism, hydrological and climatic factors, and human disturbance are main drivers regulating the aquatic carbon emissions

          • Dynamics of CO 2 and CH 4 evasion from inland waters in China's climate‐sensitive and anthropogenically disturbed regions are understudied

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          Most cited references155

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          A blueprint for blue carbon: toward an improved understanding of the role of vegetated coastal habitats in sequestering CO2

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            Plumbing the Global Carbon Cycle: Integrating Inland Waters into the Terrestrial Carbon Budget

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              Global carbon dioxide emissions from inland waters.

              Carbon dioxide (CO2) transfer from inland waters to the atmosphere, known as CO2 evasion, is a component of the global carbon cycle. Global estimates of CO2 evasion have been hampered, however, by the lack of a framework for estimating the inland water surface area and gas transfer velocity and by the absence of a global CO2 database. Here we report regional variations in global inland water surface area, dissolved CO2 and gas transfer velocity. We obtain global CO2 evasion rates of 1.8(+0.25)(-0.25)  petagrams of carbon (Pg C) per year from streams and rivers and 0.32(+0.52)(-0.26)  Pg C yr(-1) from lakes and reservoirs, where the upper and lower limits are respectively the 5th and 95th confidence interval percentiles. The resulting global evasion rate of 2.1 Pg C yr(-1) is higher than previous estimates owing to a larger stream and river evasion rate. Our analysis predicts global hotspots in stream and river evasion, with about 70 per cent of the flux occurring over just 20 per cent of the land surface. The source of inland water CO2 is still not known with certainty and new studies are needed to research the mechanisms controlling CO2 evasion globally.
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                Author and article information

                Contributors
                Journal
                Journal of Geophysical Research: Biogeosciences
                JGR Biogeosciences
                2169-8953
                2169-8961
                February 2024
                February 24 2024
                February 2024
                : 129
                : 2
                Affiliations
                [1 ] Department of Geography The University of Hong Kong Hong Kong China
                Article
                10.1029/2023JG007675
                9bc03895-b31e-4c2b-a1b2-4875f532d724
                © 2024

                http://creativecommons.org/licenses/by-nc/4.0/

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