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Work package 1

The pelagic realm

The changes in the North and Baltic Seas during the Anthropocene and their effects on their carbon stores and carbon exchange are to be examined in work package (WP) 1. An increase in total alkalinity (TA) can facilitate seasonal or long-term (> 1 year) CO2 uptake. As a result, carbon storage and export to the deep sea via the shelf pump can be increased, and the effect of atmospheric ocean acidification can be weakened.

In WP 1, new methods are to be applied that directly record the CO2 fluxes on the coast. This is intended to circumvent the uncertainty in the parameterization of the gas transfer and to create a data set that is representative over time (including the variability from hourly to seasonal scales). In addition, the representation for the model is to be made easier so that the CO2 fluxes measured at this location can be scaled up to the entire coastal region.

For this purpose, the Coastal Research Center of the NLWKN provides, among other things, ship-based data for the North Sea, Wadden Sea and estuaries. In addition, precise and high-resolution ship-based transect data of the shipping area on biogeochemistry, nutrients and, in particular, relevant parameters of the carbonate system are collected and validated.

Objectives


  • Understanding the role of anthropogenic influences on physical and biogeochemical factors that regulate the uptake and storage capacity of CO2 in the water column
  • Influence of TA changes on carbon uptake
  • Characterization of the influence of the assimilation of sulfur on carbon storage as a more resistant, dissolved organic material
  • Input of data from nature measurements into the bidirectionally coupled hydrodynamic-biogeochemical model system FVCOM / ERGOM (e.g. for calibration) (WP 3)

Reasons for change of total alkalinity (TA) in the Baltic Sea as well as past and future effects on carbon storage and export as well as gas exchange with the atmosphere

Work package 1.1 deals in detail with the potential drivers of the recently identified long-term changes in total alkalinity (TA), including anthropogenic eutrophication and potentially increased weathering. The focus here is on the processes along the gradients from land to sea and the gradients at the redox interfaces.

Objectives


  • Update of the available data on inorganic carbon and inputs into the Baltic Sea
  • Carrying out trend analyzes of total alkalinity (TA) to clarify the significance of external vs. internal sources of alkalinity
  • Assessment of the data on the carbon system with regard to the changed storage capacity and the induced change in the carbon dioxide exchange with the atmosphere
  • Investigation of the carbon system through field expeditions, the observation network in the Baltic Sea and sampling as a supplement to the regular monitoring trips (Baltic Sea monitoring and IOW long-term data collection)
  • Identification of inconsistencies (e.g. systematic errors due to the contribution of organic alkalinity) through overdetermination of the CO2 system and the characterization of stable isotopes
  • Assessment and improvement of the functioning and possible shortcomings of the description of the inorganic carbon system and the source description in the current ERGOM model
  • Operation of the model in an environment with and without a scenario of anthropogenic changes in alkalinity
  • Assessment of changes and variability in surface pCO2 with potential for better verification of the AP 3 model framework

Separation of long-term total alkalinity (TA) trends from seasonal productivity patterns

Objectives


    Sulfurization as a mechanism for storing carbon as a resistant dissolved organic material (DOM)

    Objectives


      Understanding the role of physical processes in the CO2 exchange between atmosphere and ocean along the gradient from land to sea and its sensitivity to climate change

      Objectives


        In-situ pelagic processes and pelagic-benthic coupling as a modulator of alkalinity

        Objectives