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Recent trends in the chemistry of major northern rivers signal widespread Arctic change
Tank, Suzanne E.; McClelland, James W.; Spencer, Robert G. M.; Shiklomanov, Alexander I.; Suslova, Anya; Moatar, Florentina; Amon, Rainer M. W.; Cooper, Lee W.; Elias, Greg; Gordeev, Vyacheslav V.; Guay, Christopher; Gurtovaya, Tatiana Yu.; Kosmenko, Lyudmila S.; Mutter, Edda A.; Peterson, Bruce J.; Peucker-Ehrenbrink, Bernhard; Raymond, Peter A.; Schuster, Paul F.; Scott, Lindsay; Staples, Robin; Striegl, Robert G.; Tretiakov, Mikhail; Zhulidov, Alexander V.; Zimov, Nikita; Zimov, Sergey; Holmes, Robert M. (2023). Recent trends in the chemistry of major northern rivers signal widespread Arctic change. Nature Geoscience 16(9): 789-796. https://dx.doi.org/10.1038/s41561-023-01247-7
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, more
Related to:
Lacroix, F. (2023). Arctic rivers tell tales of change. Nature Geoscience 16(9): 760-761. https://dx.doi.org/10.1038/s41561-023-01248-6, more
Peer reviewed article  

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Keyword
    Marine/Coastal

Abstract
    Rivers integrate processes occurring throughout their watersheds and are therefore sentinels of change across broad spatial scales. River chemistry also regulates ecosystem function across Earth’s land–ocean continuum, exerting control from the micro- (for example, local food web) to the macro- (for example, global carbon cycle) scale. In the rapidly warming Arctic, a wide range of processes—from permafrost thaw to biological uptake and transformation—might reasonably alter river water chemistry. Here we use data from major rivers that collectively drain two-thirds of the Arctic Ocean watershed to assess widespread change in biogeochemical function within the pan-Arctic basin from 2003 to 2019. While the oceanward flux of alkalinity and associated ions increased markedly over this time frame, nitrate and other inorganic nutrient fluxes declined. Fluxes of dissolved organic carbon showed no overall trend. This divergence in response indicates the perturbation of multiple processes on land, with implications for biogeochemical cycling in the coastal ocean. We anticipate that these findings will facilitate refinement of conceptual and numerical models of current and future functioning of Arctic coastal ecosystems and spur research on scale-dependent change across the river-integrated Arctic domain.

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