Open AccessSubsea permafrost carbon stocks and climate change sensitivity estimated by expert assessment
Author(s) -
Sayedeh Sara Sayedi,
Benjamin W. Abbott,
Brett F. Thornton,
Jennifer Frederick,
Jorien E. Vonk,
Paul Overduin,
Christina Schädel,
Edward A. G. Schuur,
Annie Bourbonnais,
Nikita Demidov,
А. В. Гаврилов,
Shengping He,
Gustaf Hugelius,
Martin Jakobsson,
Miriam C. Jones,
DongJoo Joung,
Gleb Kraev,
R. W. Macdonald,
A. David McGuire,
Cuicui Mu,
Matt OʹRegan,
K. M. Schreiner,
Christian Stranne,
Elena Pizhankova,
Alexander Vasiliev,
Sebastian Westermann,
J. P. Zarnetske,
Tingjun Zhang,
Mehran Ghandehari,
Sarah Baeumler,
Brian Brown,
Rebecca J. Frei
Publication year - 2020
Publication title -
environmental research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.37
H-Index - 124
ISSN - 1748-9326
DOI - 10.1088/1748-9326/abcc29
Subject(s) - permafrost , subsea , climate change , environmental science , arctic , representative concentration pathways , total organic carbon , hydrology (agriculture) , oceanography , climatology , physical geography , climate model , geology , environmental chemistry , geography , chemistry , geotechnical engineering
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.