The Nansen Legacy Project Blog

In the darkness of the polar night, the Nansen Legacy searches for oceanographic moorings, which have been out in the sea for the past one to two years, and that have recorded important information to study changes in the waters east and north of Svalbard.
In the darkness of the polar night, the Nansen Legacy searches for oceanographic moorings, which have been out in the sea for the past one to two years, and that have recorded important information to study changes in the waters east and north of Svalbard.

Searching in the dark

Published

On a cruise with RV Kronprins Haakon in the northern Barents Sea in the dark, we are looking for two things; purely practical for oceanographic instrument moorings that have been out and doing measurements in the ocean for one to two years, and which will now be retrieved from the depths of the ocean. Scientifically, we are looking for answers to where the warmest water in the area comes from. The measurements made by the instruments on the moorings that are now being picked up, will help us find answers to this scientific question.

The cruise covers two areas; the inner northern Barents Sea and the continental shelf slope towards the deep Arctic Ocean. In the Barents Sea, the Nansen Legacy has had moorings in four strategic locations since the fall of 2018. These are areas that have deeper connection, either to the Atlantic-influenced part of the south and west, or to the warm current that follows the topography on the north side. The projects A-TWAIN and SIOS-InfraNor have moorings that cover the inflow of warm Atlantic water going west and then north of Svalbard. Together, these new datasets will give us a much better understanding of seasonal variations in temperature and water exchange between the different areas, and the mechanisms that control the changes. In addition, the data will be valuable for interpreting observations of biogeochemistry and marine biology, as well as checking how good the ocean and sea-ice models for the area are. In addition to recovering and deploying moorings, we make measurements of salt content, temperature and ocean currents at several locations to complement the data from the instrument moorings into a larger geographical context.

When an oceanographic mooring is safely on board after standing for one to two years in the ocean, it is time for maintenance of the measuring instruments before deploying them back in the sea.
When an oceanographic mooring is safely on board after standing for one to two years in the ocean, it is time for maintenance of the measuring instruments before deploying them back in the sea.

This year there has been more ice in the Barents Sea than in a long time. The area we are in when this is written north of Kvitøya - was only ice-free for a couple of weeks in October. Getting the instrument moorings up can be challenging when we first have to clear a larger area for drifting sea ice with the ship. Fortunately, so far, things have gone well, thanks to skilled instrument engineers and the excellent crew of RV Kronprins Haakon. We have recovered six moorings so far, but many more to go. Earlier scientific cruises on other vessels this year cruises did not manage to pick up some of these moorings due to heavy ice conditions. Our cruise is the last of the year with personnel trained for such rig work. We have therefore been asked to pick up some extra moorings north of Svalbard for institutions we collaborate with, something we are happy to do. Collaboration is essential here outside the beaten track, and next time it may be us who will need assistance.

The atmosphere on board RV Kronprins Haakon is good. At the beginning of the cruise, in the middle of the Barents Sea, there was a full moon and a skim light along the southern horizon in the middle of the day. Now that a week has passed and we are at 81 degrees north, it is almost dark even at noon. Nevertheless, as we break further north, in the ship's powerful floodlights we can clearly see the contrasts between thin, newly formed ice and thicker, older ice with light snow cover and polar bear tracks.

Map of dominant currents in the European part of the Arctic Ocean (red arrows indicate the flow of warm Atlantic water inside the Arctic Ocean, blue arrows indicate the flow of colder Arctic water out of the Arctic Ocean, green arrows indicate flow of Norwegian coastal water), and the exploration areas for the ongoing expedition east and north of Svalbard (white boxes). The ice spread in 1981 and 2017 is indicated respectively by a black and white line in the Barents Sea.
Map of dominant currents in the European part of the Arctic Ocean (red arrows indicate the flow of warm Atlantic water inside the Arctic Ocean, blue arrows indicate the flow of colder Arctic water out of the Arctic Ocean, green arrows indicate flow of Norwegian coastal water), and the exploration areas for the ongoing expedition east and north of Svalbard (white boxes). The ice spread in 1981 and 2017 is indicated respectively by a black and white line in the Barents Sea.

About the blog

Welcome to a journey through the Arctic!
This blog is writtten by researchers and participants linked to The Nansen Legacy Project. They will share their experiences and knowledge from research cruises in the Barents Sea.
The research vessel F/F «Kronprins Haakon» gives unique opportunities to explore the rapidly changing climate and ecosystems in the Arctic. To ensure a sustainable management of the Northern Barents Sea and the adjacent Arctic Basin throughout the 21st century a new knowledge base is required.

(Top picture: Christian Morel / www.christianmorel.net / The Nansen Legacy)