Subsea permafrost carbon stocks and climate change sensitivity estimated by expert assessment

The continental shelves of the Arctic Ocean and surrounding seas contain large stocks of organic matter (OM) and methane (CH 4 ), representing a potential ecosystem feedback to climate change not included in international climate agreements. We performed a structured expert assessment with 25 permaf...

Full description

Bibliographic Details
Published in:Environmental Research Letters
Main Authors: Sayedi, Sayedeh Sara, Abbott, Benjamin W., Thornton, Brett F., Frederick, Jennifer M., Vonk, Jorien E., Overduin, Paul, Schädel, Christina, Schuur, Edward A.G., Bourbonnais, Annie, Demidov, Nikita, Gavrilov, Anatoly, He, Shengping, Hugelius, Gustaf, Jakobsson, Martin, Jones, Miriam C., Joung, Dong Joo, Kraev, Gleb, Macdonald, Robie W., David McGuire, A., Mu, Cuicui, O’Regan, Matt, Schreiner, Kathryn M., Stranne, Christian, Pizhankova, Elena, Vasiliev, Alexander, Westermann, Sebastian, Zarnetske, Jay P., Zhang, Tingjun, Ghandehari, Mehran, Baeumler, Sarah, Brown, Brian C., Frei, Rebecca J.
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://research.vu.nl/en/publications/9b9bf5fc-1188-4e54-bca5-5af1806847ed
https://doi.org/10.1088/1748-9326/abcc29
https://hdl.handle.net/1871.1/9b9bf5fc-1188-4e54-bca5-5af1806847ed
http://www.scopus.com/inward/record.url?scp=85099398855&partnerID=8YFLogxK
http://www.scopus.com/inward/citedby.url?scp=85099398855&partnerID=8YFLogxK
Description
Summary:The continental shelves of the Arctic Ocean and surrounding seas contain large stocks of organic matter (OM) and methane (CH 4 ), representing a potential ecosystem feedback to climate change not included in international climate agreements. We performed a structured expert assessment with 25 permafrost researchers to combine quantitative estimates of the stocks and sensitivity of organic carbon in the subsea permafrost domain (i.e. unglaciated portions of the continental shelves exposed during the last glacial period). Experts estimated that the subsea permafrost domain contains ∼560 gigatons carbon (GtC; 170–740, 90% confidence interval) in OM and 45 GtC (10–110) in CH 4 . Current fluxes of CH 4 and carbon dioxide (CO 2 ) to the water column were estimated at 18 (2–34) and 38 (13–110) megatons C yr − 1 , respectively. Under Representative Concentration Pathway (RCP) RCP8.5, the subsea permafrost domain could release 43 Gt CO 2 -equivalent (CO 2 e) by 2100 (14–110) and 190 Gt CO 2 e by 2300 (45–590), with ∼30% fewer emissions under RCP2.6. The range of uncertainty demonstrates a serious knowledge gap but provides initial estimates of the magnitude and timing of the subsea permafrost climate feedback.