Winter fluxes determine the annual carbon balance of an unmanaged subarctic drained peatland

dc.contributor.authorSalimi, Asra
dc.contributor.authorSigurdsson, Bjarni D.
dc.contributor.authorBjarnadottir, Brynhildur
dc.contributor.authorFeng, Chenxin
dc.contributor.authorÓskarsson, Hlynur
dc.contributor.authorMammarella, Ivan
dc.contributor.departmentFaculty of Education
dc.date.accessioned2026-10-05T14:50:01Z
dc.date.available2026-10-05T14:50:01Z
dc.date.issued2026-06-22
dc.descriptionPublisher Copyright: © 2026 Asra Salimi et al.en
dc.description.abstractPeatlands are critical components of the global carbon (C) cycle, storing large amounts of soil organic carbon (SOC). However, drainage substantially alters their carbon exchange and hydrological functioning, often converting them into net carbon dioxide (CO2) sources. This study presents the first year-round, ecosystem-scale Eddy Covariance (EC) assessment of CO2 dynamics from an unmanaged drained peatland in western Iceland, originally drained in the early 1960s. Two years of continuous EC measurements were collected alongside high-resolution environmental data, including solar radiation, air and soil temperatures, soil water content, and groundwater level. Several multispectral drone flights were also conducted during the study period, which provided seasonal NDVI-based estimates of canopy greenness. The two study years differed markedly in annual weather during the growing season (GS), with 2023 GS being unusually warm and dry, while 2024 GS was cold and wet. Despite these contrasts, annual net ecosystem exchange (NEE) remained similar between the 2 years. The annual NEE was dominated by non-growing-season (NGS) respiration, which highlighted the necessity for year-round measurements. Overall, the site remained a persistent CO2 source, emitting 4.1–4.4 tCO2-Cha-1 yr-1 nearly 60 years after drainage. Temperature exerted the strongest control on ecosystem respiration (Reco), while gross primary production (GPP) responded primarily to seasonal irradiance and NDVI. A compensatory mechanism was observed during the warm year (2023) at this relatively cool site, where warming-induced increases in Reco were offset by an enhanced GPP, resulting in a relatively stable annual NEE despite meteorological contrasts. Soil moisture and vapor pressure deficit played only minor roles under these cool and moist conditions. These findings highlight the need for continued monitoring of unmanaged drained peatlands to better quantify their contribution to regional greenhouse gas budgets.en
dc.description.versionPeer revieweden
dc.format.extent25
dc.format.extent5711781
dc.format.extent4011-4035
dc.identifier.citationSalimi, A, Sigurdsson, B D, Bjarnadottir, B, Feng, C, Óskarsson, H & Mammarella, I 2026, 'Winter fluxes determine the annual carbon balance of an unmanaged subarctic drained peatland', Biogeosciences, vol. 23, no. 12, pp. 4011-4035. https://doi.org/10.5194/bg-23-4011-2026en
dc.identifier.doi10.5194/bg-23-4011-2026
dc.identifier.issn1726-4170
dc.identifier.other250389837
dc.identifier.other4baabaac-236d-4899-9598-bbd3cb3fc539
dc.identifier.other105042525198
dc.identifier.urihttps://hdl.handle.net/20.500.11815/8547
dc.language.isoen
dc.relation.ispartofseriesBiogeosciences; 23(12)en
dc.relation.urlhttps://www.scopus.com/pages/publications/105042525198en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.subjectPeatlandsen
dc.subjectSub-Arcticen
dc.subjectCarbon balanceen
dc.subjectEcology, Evolution, Behavior and Systematicsen
dc.subjectEarth-Surface Processesen
dc.titleWinter fluxes determine the annual carbon balance of an unmanaged subarctic drained peatlanden
dc.type/dk/atira/pure/researchoutput/researchoutputtypes/contributiontojournal/articleen

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