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Substantial decrease in CO2 emissions from Chinese inland waters due to global change

Lishan Ran (), David E. Butman, Tom J. Battin, Xiankun Yang (), Mingyang Tian, Clément Duvert, Jens Hartmann, Naomi Geeraert and Shaoda Liu
Additional contact information
Lishan Ran: The University of Hong Kong
David E. Butman: University of Washington
Tom J. Battin: Stream Biofilm and Ecosystem Research Laboratory, School of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne
Xiankun Yang: Guangzhou University
Mingyang Tian: Guangzhou University
Clément Duvert: Charles Darwin University
Jens Hartmann: Institute for Geology, Center for Earth System Research and Sustainability (CEN), Universität Hamburg
Naomi Geeraert: The University of Hong Kong
Shaoda Liu: Beijing Normal University

Nature Communications, 2021, vol. 12, issue 1, 1-9

Abstract: Abstract Carbon dioxide (CO2) evasion from inland waters is an important component of the global carbon cycle. However, it remains unknown how global change affects CO2 emissions over longer time scales. Here, we present seasonal and annual fluxes of CO2 emissions from streams, rivers, lakes, and reservoirs throughout China and quantify their changes over the past three decades. We found that the CO2 emissions declined from 138 ± 31 Tg C yr−1 in the 1980s to 98 ± 19 Tg C yr−1 in the 2010s. Our results suggest that this unexpected decrease was driven by a combination of environmental alterations, including massive conversion of free-flowing rivers to reservoirs and widespread implementation of reforestation programs. Meanwhile, we found increasing CO2 emissions from the Tibetan Plateau inland waters, likely attributable to increased terrestrial deliveries of organic carbon and expanded surface area due to climate change. We suggest that the CO2 emissions from Chinese inland waters have greatly offset the terrestrial carbon sink and are therefore a key component of China’s carbon budget.

Date: 2021
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DOI: 10.1038/s41467-021-21926-6

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