Comparisons of dissolved organic matter and its optical characteristics in small low and high Arctic catchments

• Published in: Biogeosciences
• Main Authors: Coch, Caroline, Juhls, Bennet, Lamoureux, Scott F., Lafrenièr, Melissa J., Fritz, Michael, Heim, Birgit, Lantuit, Hugues
• Format: Article in Journal/Newspaper
• Language: English
• Published: Zenodo 2019
• Subjects: Arctic; DOM; catchment; permafrost; optical characteristics; Climate change; Nunavut; Melville Island; Yukon
• Online Access: https://doi.org/10.5194/bg-16-4535-2019

Climate change is affecting the rate of carbon cycling, particularly in the Arctic. Permafrost degradation through deeper thaw and physical disturbances results in the release of carbon dioxide and methane to the atmosphere andto anincrease inlateral dissolved organic matter (DOM) fluxes. Whereas riverine DOM fluxes of the large Arctic rivers are well assessed, knowledge is limited with regard to small catchments that cover more than 40% of the Arctic drainage basin. Here, we use absorption measurements to characterize changes in DOM quantity and quality in a lowArctic(HerschelIsland,Yukon,Canada)andahighArctic (Cape Bounty, Melville Island, Nunavut, Canada) setting with regard to geographical differences, impacts of permafrost degradation, and rainfall events. We find that DOM quantity and quality is controlled by differences in vegetation cover and soil organic carbon content (SOCC). The low Arctic site has higher SOCC and greater abundance of plant material resulting in higher chromophoric dissolved organic matter (cDOM) and dissolved organic carbon (DOC) than in the high Arctic. DOC concentration and cDOM in surface waters at both sites show strong linear relationships similar to the one for the great Arctic rivers. We used the optical characteristics of DOM such as cDOM absorption, specific ultraviolet absorbance (SUVA), ultraviolet (UV) spectral slopes (S275–295), and slope ratio (SR) for assessing quality changes downstream, at base flow and storm flow conditions, and in relation to permafrost disturbance. DOM in streams at both sites demonstrated optical signatures indicative of photodegradation downstream processes, even over short distances of 2000m. Flow pathways and the connected hydrological residence time control DOM quality. Deeper flow path ways allow the Export of permafrost-derived DOM (i.e. from deeper in the active layer), whereas shallow pathways with shorter residence times lead to the export of fresh surface- and near-surface-derived DOM. Compared to the large Arctic rivers, DOM quality ...