Project Details
Projekt Print View

The biogeochemistry of ocean-ice interaction around Greenland

Applicant Dr. Mark Hopwood
Subject Area Oceanography
Term from 2019 to 2022
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 422642301
 
Final Report Year 2024

Final Report Abstract

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.

Publications

 
 

Additional Information

Textvergrößerung und Kontrastanpassung