Projektnamn: SkaMix@UGOT
Huvudforskare: Göran Broström
Om projektet (på engelska):
This project will be carried out in collaboration with German, Swedish, and Norwegian partners. Germany partners have applied for ship-time for two medium sized research vessels (RV Elisabeth Mann Borghese and RV Heinke). We aim to take part in this international experiment with RV Skagerak.
SkaMix is an international effort to investigate water mass transformation in Skagerak. In 2025, two German Ships and RV Skagerak will do synchronized detailed investigation of mixing dynamics and drift patterns. The GU team will focus on southern Skagerrak and the Kattegat-Skagerrak front. In addition, we want to combine the 2025 expedition with a follow up expedition in 2026 that focuses on mixing conditions and transport pathways in Kattegat. We will make use of other GU infrastructure where available, such as gliders, autonomous surface vehicles (USVs) to supplement the ship-based observations. Ship funding is secured for 2025 and 2026, and we will submit a proposal to FORMAS to support these expeditions.
The central objective of SkaMix is to obtain a quantitative understanding of water mass transformation processes in a complex ocean mixing hotspot region, the Skagerrak that connects the Baltic Sea and the Kattegat with the North Sea. The processes in the Skagerrak as a prototype water mass transformation region determine the fate of at least three inflowing water masses (Baltic outflow, Jutland current, Atlantic water) that create two outflowing water masses (Norwegian Coastal Current, Baltic inflow). Those outflowing water masses with their hydrographic signature (temperature, salinity) and biogeochemical constituents (e.g., oxygen, nutrients, organisms) are source waters for large water bodies such as the Baltic Sea and the Norwegian Sea that determine their dynamics and ecosystem processes.
The key research questions of SkaMix are:
1. What are the inflowing and outflowing currents in the Skagerrak and what is the T-S signature and their strength? How does this vary spatially and temporally? , as function of time and space?
2. What are the major drivers for the variability and trends of the transports of these currents?
3. What are the major processes that drive the water mass transformation inside the Skagerrak?
4. What are the pathways of water masses inside the Skagerrak and what are the residence times of these water masses?
5. How can the results from the Skagerrak expedition be generalized for other oceanic water mass transformation hotspots?
6. How can the numerical framework of this region be transferred to other mixing hotspots?