Articles | Volume 19, issue 24
https://doi.org/10.5194/bg-19-5973-2022
https://doi.org/10.5194/bg-19-5973-2022
Research article
 | 
22 Dec 2022
Research article |  | 22 Dec 2022

Nitrate isotope investigations reveal future impacts of climate change on nitrogen inputs and cycling in Arctic fjords: Kongsfjorden and Rijpfjorden (Svalbard)

Marta Santos-Garcia, Raja S. Ganeshram, Robyn E. Tuerena, Margot C. F. Debyser, Katrine Husum, Philipp Assmy, and Haakon Hop

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Cited articles

Adakudlu, M., Andersen, J., Bakke, J., Beldring, S., Benestad, R., Bilt, W. V. D., and Wong, W. K.: Climate in Svalbard 2100 – a knowledge base for climate adaptation. Norway, Norwegian Centre of Climate Services (NCCS) for Norwegian Environment Agency (Miljødirektoratet), 208 pp., NCCS report, Norwegian Centre for Climate Services (NCCS) for Norwegian Environment Agency (Miljødirektoratet), https://doi.org/10.25607/OBP-888, 2019. 
Altabet, M. A. and Francois, R.: Nitrogen isotope biogeochemistry of the Antarctic Polar Frontal Zone at 170 W, Deep-Sea Res. Pt. II, 48, 4247–4273, https://doi.org/10.1016/S0967-0645(01)00088-1, 2001. 
Ansari, A. H., Hodson, A J, Heaton, T. H. E., Kaiser, J., and Marca-Bell, A.: Stable isotopic evidence for nitrification and denitrification in a High Arctic glacial ecosystem, Biogeochemistry, 113, 341–357, https://doi.org/10.1007/s10533-012-9761-9, 2013. 
Arctic Climate Impact Assessment (ACIA).: Arctic Climate Impact Assessment, 1042 pp., Cambridge Univ. Press, Cambridge, UK, ISBN: 13 978-0-521-86509, 2005. 
Beszczynska-Moller, A., Fahrbach, E., Schauer, U., and Hansen, E.: Variability in Atlantic water temperature and transport at the entrance to the Arctic Ocean, 19972010, ICES J. Mar. Sci., 69, 852–863, https://doi.org/10.1093/ICESJMS/FSS056, 2012. 
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Terrestrial sources of nitrate are important contributors to the nutrient pool in the fjords of Kongsfjorden and Rijpfjorden in Svalbard during the summer, and they sustain most of the fjord primary productivity. Ongoing tidewater glacier retreat is postulated to favour light limitation and less dynamic circulation in fjords. This is suggested to encourage the export of nutrients to the middle and outer part of the fjord system, which may enhance primary production within and in offshore areas.
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