The ocean breathes
Friederike Fröb defends on Tuesday, 27th of June 2017 her PhD dissertation at the University of Bergen with the title: “Climate controlled mechanisms of subpolar North Atlantic carbon uptake”.
Since the industrial revolution in the mid 18th century, atmospheric CO2 concentrations have increased almost exponentially, mainly caused by carbon emissions from fossil fuel burning and land use changes. A large fraction of the human-induced CO2 has been stored in the ocean carbon sink. The oceanic uptake of CO2 thus mitigates climate change, however, the uptake efficiency is highly variable in space and time due to complex interactions between atmospheric, hydrographic and biogeochemical processes.
The focus region of the thesis is the subpolar North Atlantic, with particular emphasis on the Irminger Sea, as the North Atlantic plays a dominant role for global carbon uptake. In the thesis, carbon cycle changes in the interior and surface ocean are documented through the 1990s and 2000s in relation to large-scale circulation changes, atmospheric forcing mechanisms and winter mixing processes as well as the increasing atmospheric CO2 concentrations. Further, ocean acidification over the past 25 years is discussed. The results are based on observational data collected during dedicated scientific cruises as well as by autonomous sampling systems installed on Voluntary Observing Ships.
This thesis shows that the carbon cycle in the North Atlantic undergoes significant spatial and temporal variability. The long-term trends of carbon cycle processes are dominated by the uptake of anthropogenic CO2. However, over short periods of time the large variability of internal processes can in fact mask the anthropogenic forcing. Therefore, when the magnitude, trends and variability of carbon uptake processes are discussed, the natural carbon cycle should also be taken into consideration.
Some pictures from a cruise to the Irminger Sea in 2015.