Canopy-Mediated Climate Feedbacks in the Boreal Continuous Permafrost Zone | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Article Canopy-Mediated Climate Feedbacks in the Boreal Continuous Permafrost Zone Simone Stuenzi, Guido Grosse, Frederieke Miesner, Sebastian Westermann, and 1 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-7961174/v1 This work is licensed under a CC BY 4.0 License Status: Under Review Version 1 posted You are reading this latest preprint version Abstract Boreal forests, covering approximately a quarter of the continuous permafrost zone, store relatively modest aboveground carbon, but thermally protect vast soil organic carbon pools. Using a process-based model to compare seasonal thaw depths under forested and bare-ground scenarios, we quantify distinct canopy thermal insulation capacities of deciduous needleleaf, evergreen needleleaf, and deciduous broadleaf canopies on permafrost thermal dynamics. Canopy buffering maintains approximately 59 Pg of carbon in a frozen state, which equals 32% of the total forested permafrost carbon pool and far exceeds boreal biomass stocks (7-19 Pg). Canopy changes could mobilize this frozen SOC through gradual thaw (40 Pg) and rapid thermokarst collapse (19 Pg). While forest loss sacrifices biomass carbon stocks, resulting thaw would expose orders of magnitude more SOC from previously frozen reservoirs, revealing a critical asymmetry. Forest conservation strategies in continuous permafrost zones must account for canopy-mediated thermal protection of frozen SOC, which far exceeds its biomass carbon sequestration capacity. Earth and environmental sciences/Climate sciences/Cryospheric science Earth and environmental sciences/Ecology/Ecosystem services Earth and environmental sciences/Environmental sciences/Environmental impact Global Warming Impact Carbon stock Boreal forest Permafrost Full Text Additional Declarations There is NO Competing Interest. Supplementary Files SI.pdf Supplementary Information: Canopy-Mediated Climate Feedbacks in the Boreal Continuous Permafrost Zone Cite Share Download PDF Status: Under Review Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. We do this by developing innovative software and high quality services for the global research community. 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