Diffusive and advective cross-frontal fluxes of inorganic nutrients and dissolved inorganic carbon in the Barents Sea in autumn

Author:

Koenig ZoeORCID,Fer Ilker,Chierici Melissa,Fransson AgnetaORCID,Jones ElizabethORCID,Kolås Eivind H.ORCID

Funder

Norges Forskningsråd

Universitetet i Tromsø

Publisher

Elsevier BV

Subject

Geology,Aquatic Science

Reference60 articles.

1. Quantifying the influence of Atlantic heat on Barents Sea ice variability and retreat;Årthun;J. Clim.,2012

2. Leads in Arctic pack ice enable early phytoplankton blooms below snow-covered sea ice;Assmy;Sci. Rep.,2017

3. Observed Atlantification of the Barents Sea causes the Polar Front to limit the expansion of winter sea ice;Barton;J. Phys. Oceanogr.,2018

4. Impact of biogeochemical processes and environmental factors on the calcium carbonate saturation state in the Circumpolar Flaw lead in the Amundsen Gulf, Arctic Ocean;Chierici;J. Geophys. Res.: Oceans,2011

5. Arctic chemical oceanography at the edge: Focus on carbonate chemistry;Chierici,2018

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