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  • 1. Denfeld, Blaize A.
    et al.
    Baulch, Helen M.
    del Giorgio, Paul A.
    Hampton, Stephanie E.
    Karlsson, Jan
    A synthesis of carbon dioxide and methane dynamics during the ice-covered period of northern lakes2018In: Limnology and Oceanography Letters, E-ISSN 2378-2242, Vol. 3, no 3, p. 117-131Article in journal (Refereed)
    Abstract [en]

    The ice-covered period on lakes in the northern hemisphere has often been neglected or assumed to have less importance relative to the open water season. However, recent studies challenge this convention, suggesting that the winter period is more dynamic than previously thought. In this review, we synthesize the current understanding of under-ice carbon dioxide (CO2) and methane (CH4) dynamics, highlighting the annual importance of CO2 and CH4 emissions from lakes at ice-melt. We compiled data from 25 studies that showed that the ice-melt period represents 17% and 27% of the annual CO2 and CH4 emissions, respectively. We also found evidence that the magnitude and type of emission (i.e., CO2 and CH4) varies with characteristics of lakes including geographic location, lake morphometry, and physicochemical conditions. The scarcity of winter and spring carbon data from northern lakes represents a major gap in our understanding of annual budgets in these lakes and calls for future research during this key period.

  • 2. Rocher-Ros, Gerard
    et al.
    Sponseller, Ryan A.
    Lidberg, William
    Mörth, Carl-Magnus
    Giesler, Reiner
    Landscape process domains drive patterns of CO2 evasion from river networks2019In: Limnology and Oceanography Letters, E-ISSN 2378-2242, Vol. 4, no 4, p. 87-95Article in journal (Refereed)
    Abstract [en]

    Abstract Streams are important emitters of CO2 but extreme spatial variability in their physical properties can make upscaling very uncertain. Here, we determined critical drivers of stream CO2 evasion at scales from 30 to 400?m across a 52.5 km2 catchment in northern Sweden. We found that turbulent reaches never have elevated CO2 concentrations, while less turbulent locations can potentially support a broad range of CO2 concentrations, consistent with global observations. The predictability of stream pCO2 is greatly improved when we include a proxy for soil-stream connectivity. Catchment topography shapes network patterns of evasion by creating hydrologically linked ?domains? characterized by high water-atmosphere exchange and/or strong soil-stream connection. This template generates spatial variability in the drivers of CO2 evasion that can strongly bias regional and global estimates. To overcome this complexity, we provide the foundations of a mechanistic framework of CO2 evasion by considering how landscape process domains regulate transfer and supply.

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