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Carbon and Beyond : The Biogeochemistry of Climate in a Rapidly Changing Amazon

Authors :
Covey, Kristofer
Soper, Fiona
Pangala, Sunitha
Bernardino, Angelo
Pagliaro, Zoe
Basso, Luana
Cassol, Henrique
Fearnside, Philip
Navarrete, Diego
Novoa, Sidney
Sawakuchi, Henrique
Lovejoy, Thomas
Marengo, Jose
Peres, Carlos A.
Baillie, Jonathan
Bernasconi, Paula
Camargo, Jose
Freitas, Carolina
Hoffman, Bruce
Nardoto, Gabriela B.
Nobre, Ismael
Mayorga, Juan
Mesquita, Rita
Pavan, Silvia
Pinto, Flavia
Rocha, Flavia
de Assis Mello, Ricardo
Thuault, Alice
Bahl, Alexis Anne
Elmore, Aurora
Covey, Kristofer
Soper, Fiona
Pangala, Sunitha
Bernardino, Angelo
Pagliaro, Zoe
Basso, Luana
Cassol, Henrique
Fearnside, Philip
Navarrete, Diego
Novoa, Sidney
Sawakuchi, Henrique
Lovejoy, Thomas
Marengo, Jose
Peres, Carlos A.
Baillie, Jonathan
Bernasconi, Paula
Camargo, Jose
Freitas, Carolina
Hoffman, Bruce
Nardoto, Gabriela B.
Nobre, Ismael
Mayorga, Juan
Mesquita, Rita
Pavan, Silvia
Pinto, Flavia
Rocha, Flavia
de Assis Mello, Ricardo
Thuault, Alice
Bahl, Alexis Anne
Elmore, Aurora
Publication Year :
2021

Abstract

The Amazon Basin is at the center of an intensifying discourse about deforestation, land-use, and global change. To date, climate research in the Basin has overwhelmingly focused on the cycling and storage of carbon (C) and its implications for global climate. Missing, however, is a more comprehensive consideration of other significant biophysical climate feedbacks [i.e., CH4, N2O, black carbon, biogenic volatile organic compounds (BV0Cs), aerosols, evapotranspiration, and albedo] and their dynamic responses to both localized (fire, land-use change, infrastructure development, and storms) and global (warming, drying, and some related to El Nino or to warming in the tropical Atlantic) changes. Here, we synthesize the current understanding of (1) sources and fluxes of all major forcing agents, (2) the demonstrated or expected impact of global and local changes on each agent, and (3) the nature, extent, and drivers of anthropogenic change in the Basin. We highlight the large uncertainty in flux magnitude and responses, and their corresponding direct and indirect effects on the regional and global climate system. Despite uncertainty in their responses to change, we conclude that current warming from non-CO2 agents (especially CH4 and N2O) in the Amazon Basin largely offsets- and most likely exceeds-the climate service provided by atmospheric CO2 uptake. We also find that the majority of anthropogenic impacts act to increase the radiative forcing potential of the Basin. Given the large contribution of less-recognized agents (e.g., Amazonian trees alone emit similar to 3.5% of all global CH4), a continuing focus on a single metric (i.e., C uptake and storage) is incompatible with genuine efforts to understand and manage the biogeochemistry of climate in a rapidly changing Amazon Basin.<br />Funding Agencies|National Geographic SocietyNational Geographic Society; Rolex partnership; National Geographic Society research grantNational Geographic Society; FAPESPFundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2018/14006-4, 2018/14423-4, 2014/508489]; National Coordination for High Level Education and Training (CAPES) [88887.136402-00INCT]; National Institute of Science and Technology for Climate Change Phase 2 (CNPq) [465501/2014-1]; CNPqNational Council for Scientific and Technological Development (CNPq) [311103/2015-4, 429795/2016-5]; FAPEAM [708565]; INPA [PRJ15.125]; Rede Clima (INPE) FINEP [01.13.0353-00]

Details

Database :
OAIster
Notes :
application/pdf, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1280631096
Document Type :
Electronic Resource
Full Text :
https://doi.org/10.3389.ffgc.2021.618401