Preprints
https://doi.org/10.5194/egusphere-2025-4754
https://doi.org/10.5194/egusphere-2025-4754
10 Oct 2025
 | 10 Oct 2025
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Spatiotemporal Variability and Environmental Controls on Aquatic Methane Emissions in an Arctic Permafrost Catchment

Michael W. Thayne, Karl Kemper, Christian Wille, Aram Kalhori, and Torsten Sachs

Abstract. Understanding spatiotemporal dynamics and drivers of methane (CH4) fluxes from rapidly changing permafrost regions is critical for improving our understanding of such changes. Between May and August 2023 and 2024, we measured CH4 using floating chambers in a small Arctic permafrost catchment on Disko Island, Greenland. Diffusive and ebullitive fluxes were derived from 707 measurements using a semi-automated algorithm incorporating boosted regression trees and generalized additive models. Highest fluxes occurred in streams and along lakeshores associated with inlets. Diffusion processes dominated (98 %), while 2 % were split between ebullition and uptake. Median diffusive fluxes were 5.0 nmol m-2s-1, (-0.1 to 271.8), peaking at ice-break. Ebullition had a median of 939 nmol m-2s-1 (5.2–14,893), but did not impact overall fluxes. Model results suggest thaw-season fluxes reflected meteorology and soil wetness effects, later shifting to biogeochemical controls: dissolved organic matter, oxygen saturation, and pH. Spatial variability arose from patchy conditions shaped by substrate, primary producers and microbial assemblages.

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Michael W. Thayne, Karl Kemper, Christian Wille, Aram Kalhori, and Torsten Sachs

Status: open (until 21 Nov 2025)

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Michael W. Thayne, Karl Kemper, Christian Wille, Aram Kalhori, and Torsten Sachs
Michael W. Thayne, Karl Kemper, Christian Wille, Aram Kalhori, and Torsten Sachs
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Short summary
We measured >700 methane fluxes using floating chambers in a permafrost catchment on Disko Island, Greenland. Diffusion dominated emissions, while ebullition and uptake were rare. Fluxes peaked at thaw under meteorological and soil moisture control, shifting later to regulation by dissolved organic matter, oxygen saturation, and pH. Streams and lake inlets emerged as emission hotspots, providing rare process-level insight into methane cycling in an underrepresented Arctic region.
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