Acknowledgments
This work is a collaborative effort from the Global Carbon Project
Second REgional Carbon Cycle and Processes study (RECCAP2) and
contributes to the Arctic Methane and Permafrost Challenge (AMPAC). JR
and GH acknowledge support from the European Union’s Horizon 2020
Research and Innovation Programme to the Nunataryuk project (no. 773421)
and support from the AMPAC-Net project funded by the European Space
Agency (ESA). JR received additional funding from the Swedish Academy of
Science (Formas) under the grant number FR-2021/0004. EJB has received
funding from the European Union’s Horizon 2020 research and innovation
programme under Grant Agreement No 101003536 (ESM2025 - Earth System
models for the Future) and from the Joint UK BEIS/Defra Met Office
Hadley Centre Climate Programme (GA01101). Work of MEM was supported by the Academy of Finland
in the frame of the Atmosphere and Climate Competence Center (ACCC) (no.
337550). CV was supported by the Academy of Finland project MUFFIN
(grant no. 332196). CB wishes to thank the Academy of Finland (project
N-PERM - decision no. 341348, project NOCA - decision no. 314630 and the
Yedoma-N project decision no. 287469) for financial support. AMV, BMR,
SMN, JDW, and SP were funded by the Gordon and Betty Moore foundation
(grant #8414) and through funding catalyzed by the Audacious Project
(Permafrost Pathways). MAK was supported by the NSF PRFB Program
(Abstract # 2109429). TK acknowledges support through the project
Palmod, funded by the German Federal Ministry of Education and Research
(BMBF), Grant No. 01LP1921A. JGC was funded by the Australian National
Environmental Science Program (NESP2) - Climate Systems Hub. MIROC4-ACTM
inversion activity is supported by the Arctic Challenge for
Sustainability phase II (ArCS-II; JPMXD1420318865) Projects of the
Ministry of Education, Culture, Sports, Science and Technology (MEXT),
and Environment Research and Technology Development Fund
(JPMEERF21S20800) of the Environmental Restoration and Conservation
Agency of Japan. ELB considers this study a contribution to
GreenFeedBack (Greenhouse gas fluxes and earth system feedbacks) funded
by the European Union’s HORIZON research and innovation program under
grant agreement No 101056921. EAGS was funded by NSF PLR Arctic System
Science Research Networking Activities (RNA) Permafrost Carbon Network:
Synthesizing Flux Observations for Benchmarking Model Projections of
Permafrost Carbon Exchange (2019-2023) Grant#1931333.