File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

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

TitleCarbon Emissions From Chinese Inland Waters: Current Progress and Future Challenges
Authors
Keywordsanthropogenic perturbations
biogeochemical processes
CH4 emissions
Chinese inland waters
CO2 emissions
Issue Date24-Feb-2024
PublisherAmerican Geophysical Union
Citation
Journal of Geophysical Research: Biogeosciences, 2024, v. 129, n. 2 How to Cite?
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 (CO2) and methane (CH4) emission dynamics from China's inland waters in response to global change. Major drivers of CO2 and CH4 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 CO2 and CH4 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.


Persistent Identifierhttp://hdl.handle.net/10722/348243
ISSN
2023 Impact Factor: 3.7
2023 SCImago Journal Rankings: 1.459

 

DC FieldValueLanguage
dc.contributor.authorYang, Qianqian-
dc.contributor.authorChen, Shuai-
dc.contributor.authorLi, Yuxin-
dc.contributor.authorLiu, Boyi-
dc.contributor.authorRan, Lishan-
dc.date.accessioned2024-10-08T00:31:11Z-
dc.date.available2024-10-08T00:31:11Z-
dc.date.issued2024-02-24-
dc.identifier.citationJournal of Geophysical Research: Biogeosciences, 2024, v. 129, n. 2-
dc.identifier.issn2169-8953-
dc.identifier.urihttp://hdl.handle.net/10722/348243-
dc.description.abstract<p>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 (CO2) and methane (CH4) emission dynamics from China's inland waters in response to global change. Major drivers of CO2 and CH4 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 CO2 and CH4 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.</p>-
dc.languageeng-
dc.publisherAmerican Geophysical Union-
dc.relation.ispartofJournal of Geophysical Research: Biogeosciences-
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.-
dc.subjectanthropogenic perturbations-
dc.subjectbiogeochemical processes-
dc.subjectCH4 emissions-
dc.subjectChinese inland waters-
dc.subjectCO2 emissions-
dc.titleCarbon Emissions From Chinese Inland Waters: Current Progress and Future Challenges-
dc.typeArticle-
dc.identifier.doi10.1029/2023JG007675-
dc.identifier.scopuseid_2-s2.0-85185929214-
dc.identifier.volume129-
dc.identifier.issue2-
dc.identifier.eissn2169-8961-
dc.identifier.issnl2169-8953-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats