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Projekt Druckansicht

Die Biogeochemie der Ozean-Eis-Interaktion in Grönland

Antragsteller Dr. Mark Hopwood
Fachliche Zuordnung Physik, Chemie und Biologie des Meeres
Förderung Förderung von 2019 bis 2022
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 422642301
 
Erstellungsjahr 2024

Zusammenfassung der Projektergebnisse

In summary, via field studies in Disko Bay, southwest Greenland (Nuup Kangerlua and Ameralik), northeast Greenland (Nioghalvfjerdsbræ, ‘the 79° North Glacier’) and the Western Antarctic Peninsula, we characterize glaciers as important sources of the micronutrient Mn to marine budgets, and minor sources of Fe and silica. Diverging responses to glacier retreat and increasing freshwater are expected contrasting the Antarctic and Arctic. Freshwater in Greenland glacier fjords increases stratification in systems where primary production is already N-limited throughout summer, further favoring heterotrophic processes and reinforcing conditions that induce ow marine primary production. Conversely, light remains the main bottom-up driver of primary production around the WAP in summer. Runoff thereby promotes stratification with macronutrients and micronutrient (Fe and Mn) concentrations both sufficient to facilitate increased primary production under more favorable light regimes.

Projektbezogene Publikationen (Auswahl)

 
 

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