Changes in hydrological regime regulate POC export across permafrost-dominated Arctic River basins
Shiqi Liu , Ping Wang , Jingjie Yu , Renjie Zhou , Bing Bai , Olga I. Gabysheva , Natalia L. Frolova , Sergey P. Pozdniakov
Geoscience Frontiers ›› 2026, Vol. 17 ›› Issue (1) : 102208
Warming-driven acceleration of hydrological processes is altering the carbon cycle in permafrost-dominated Arctic regions, yet the underlying drivers remain unclear. This study analyzes ArcticGRO data (2003-2021) from six major Arctic rivers (Ob, Yenisei, Lena, Kolyma, Yukon, and Mackenzie) to investigate trends and spatial-temporal variations in riverine particulate organic carbon (POC). The annual POC flux from these six rivers, estimated using the Load Estimator (LOADEST), averaged 2.78 Tg. Only the Lena River showed a notable annual decrease in POC flux ( − 3.9%/yr, p < 0.001) and concentration ( − 12%/yr, p < 0.001), while the Yukon River exhibited increasing streamflow (+0.98%/yr, p < 0.001) and POC flux (+3.2%/yr, p < 0.001). POC flux variations were primarily governed by streamflow and POC concentration, with higher concentrations in spring floods period and lower during winter. Spatial differences were linked to drainage density ( Dd ) and forest coverage ( Fc ). The Yukon River basin, with a higher Dd of 0.2 km/km 2 and lower Fc approximately 24%, exhibits the highest POC concentrations (2.3 mg/L). In contrast, the Yenisei River basin has the lowest POC concentration ( ∼ 0.4 mg/L), along with a relatively low drainage density ( Dd = 0.18 km/km 2 ) and a high forest cover ( Fc = 67%). Permafrost conditions constrained riverine POC export, with isotopic evidence indicating a shift from a carbon sink to a source, as POC carbon age increased by ∼ 200 to 1700 years (4%-68%) annually, peaking in winter (700-2500 years) after 2012. Rivers with lower permafrost coverage (e.g., Ob, Yenisei), exhibit higher winter POC fluxes contributions (10%-20%), while others contributed < 5%, suggesting the role of permafrost degradation in winter carbon export. This study emphasizes the need to assess climate-driven hydrological shifts and permafrost thaw in shaping Arctic land-to-ocean carbon fluxes.
Particulate organic carbon / Arctic rivers / Permafrost degradation / Climate change / Hydrological regime
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