Day 2: Monday 22 June 2020

Things are starting to become serious on the second day. It’s time to hit the road…uhhh no – to set sail and head off for Iceland! After settling and unpacking each single box containing lab equipment such as chemicals, microscopes, small bottles, large bottles, medium bottles, tools and a lot more, R/V Sonne is released from the ropes that are tying her to the pier. Hooting solemnly to say good-bye to R/V Maria S. Merian (one of the other German research vessels), who is lying alongside to us, R/V Sonne starts her engines to cast off. But before going anywhere we need to pass the lock that keeps the (very) low tide on the mudflats out of the harbour area and ensures the under-keel clearance. I can tell you, it is quite fascinating to see such a large vessel entering such a small gap and still being overtaken by other ships – the captain certainly knows what he is doing.

It’s a tight fit, but we do fit!

We leave the lock safely and now the open ocean is waiting for us. Our journey continues and passing huge wind parks, we go north, north, north… On the way up we will cross the exclusive economic zones (EEZ) of three countries:  the Netherlands, Denmark and Norway. EEZs are those areas of the ocean that (except for some special cases) extend to 200 nm beyond the land-water-mark. According to the United Nations Convention on the Law of the Sea (UNCLOS), each country has sovereign rights in ‘their’ EEZ, meaning that no scientific operations (and no fishing, drilling etc.) is allowed to take place without permission. Thus, any research work and all its details have to be announced, depending on the country, up to 6 months in advance and approval has to be granted. Bearing this in mind and considering the Corona situation, it hasn’t been possible to apply on time for research permission in every country’s EEZ that is being passaged. Hence, there is some transit time which is very well used to get organised and plan the actions for station 1, located north-west of the Faeroe islands in the Norwegian basin. It’s just a tiny little bit south of the polar circle (65° N, 0° E)! But more on this tomorrow!

Our progress so far: we started in the port of Emden and are heading out into the North Sea

Day 1: Sunday 21 June 2020

Welcome to the IceAGE3 blog on the MerMet 17-6 cruise on R/V Sonne!

Having completed a 3-day quarantine in the hotel room with lovely service and loads of delicious meals, everyone got a negative result for the Corona test – meaning that all of us (ship’s crew, ROV team and science group) were free to board R/V Sonne for a 5-week cruise around Iceland.

Once arriving aboard, we were shown the (single!) cabins and after a short lunch break we started unpacking the containers. Such a large amount of equipment! There is the benthic sledge which is being dragged over the seafloor trying to collect representative samples of the seafloor. There is the box corer and the MUC (mulitcore), both giving us the chance to sample seafloor at distinct points to know precisely where the probe is from. Last (but certainly not least!) comes the plankton net that sweeps through the water column collecting the smallest, yet one of the most important, species in the marine food chain. For nearly every observation or measurement being made in (ocean) waters it is crucial to know three basic parameters: salinity (i.e. conductivity), temperature, and the pressure (depth) at which those measures are taken (and of course position and time, because of seasonal and temporal variations of the measures). The instrument that provides us with those important values is called a ‘CTD’ and basically consists of a steel construction holding bottles which can be opened (and closed) at certain depths to sample sea water. By knowing salinity, temperature and depth, the local sound velocity can be derived. This is, among others, essential to consider for bathymetry mapping, i.e. acoustically strobing the seafloor to get an idea about the topography. Mapping is done with a multibeam echosounder that is installed on the hull of the vessel. It operates by transmitting acoustic energy waves through the water column. They are reflected by the ocean floor and from the time the signal needs to travel back to the echosounder, the water depth can be calculated. Using the strength (intensity) of the reflected signal gives information about seafloor characteristics. Having a high-resolution map is the basis to all further operations as, to mention only one reason, we don’t want to crash the expensive equipment into a seamount (or destroy that seamount, either!).

And now, a spoiler for what is coming up in the next days/weeks: Probably the most exciting instrument on board R/V Sonne, ‘Kiel 6000’, is waiting on the quarterdeck for its launch…stay tuned if you’d like to meet him and get insights to real deep-sea science! More on this will follow!

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Here comes the kit! Loading all the equipment onto RV Sonne in the port at Emden