"This is an unforeseen consequence of climate change", says Kjetil Våge.
He has just returned from the ice edge east of Greenland. In a unique cruise led by Woods Hole Oceanographic Institution, oceanographers and meteorologists collected data from the atmosphere and the ocean. Together with researchers from the Bjerknes Centre for Climate Change and the Geophysical Institute at the University of Bergen, they traveled to a region where few ships go in winter.
While Våge and his colleagues were at sea, their analyses from a previous glider cruise were published in the journal Nature Communications. In their study, they show that reduced sea ice cover off the coast of East Greenland can lead to more overturning of the water masses. This overturning is an important component of the circulation in the Atlantic Ocean.
Researchers have previously warned that global warming can reduce the Gulf Stream and extension along the Norwegian coast. Våge's work adds a new element to the picture. Increased overturning along the coast of East Greenland may contribute to maintaining the circulation in the ocean.
"Our results show how complex the climate system and the ocean currents are, and how difficult it is to predict the consequences of global warming", says Kjetil Våge.
Ocean circulation and sinking water
The large ocean currents on Earth distribute heat between the warm tropics and the cold, polar regions. In the Atlantic, water flows northward near the surface; in the Gulf Stream and farther north between the Faroes and Scotland, into the Norwegian Sea and along the Norwegian coast. As the water cools, it becomes heavier and sinks. Then, it flows southward along the coast of Greenland and through the strait between Iceland and Greenland toward the bottom of the Atlantic.
Scientists call this the Atlantic meridional overturning circulation. It can be looked upon as a conveyor belt, where water flows northward near the surface and returns to the south at depth. The sinking of water in the north is a necessary condition for maintaining the overturning circulation.
This is the background for the theory that global warming may reduce the overturning circulation, and then also the extension of the Gulf Stream along the Norwegian coast. When the air gets warmer, the surface water will not be cooled as much as before and then not sink as efficiently. As a result, the surface current flowing northward will also be reduced.
Kjetil Våge's new results show that this reduction may be counteracted as more water sinks outside the east coast of Greenland. In this region, the water flows southward, both at the surface and farther down. As long as there is ice on the water, it is protected against the cold winter air above. When the ice disappears, the water is cooled and sinks.
"It may seem counterintuitive that a warmer climate generates colder sea water", says Kjetil Våge.
So far, he can not tell how large the effect of increased overturning off the coast of Greenand will be, compared to the effect of reduced overturning in the Norwegian Sea. But the coast of Greenland is long, and so is the stretch where southward flowing water will be exposed. For that reason, he believes the contribution may be significant.
Storms are common in the Greenland Sea and the Iceland Sea in winter. Going there in summer is normally seen as a better way to ensure you get the measurements you need. As a result, there is very little data from the region outside the summer months. It has been assumed that little downwelling and overturning occur there. This may simply be due to a lack of winter observations. According to Kjetil Våge, most of the sinking takes place during winter, after strong northerly winds have plowed the surface water away and cold air can cool the ocean.
In summer, with calmer weather, there is more fresh and light water at the surface than in winter. Less dense water on top of denser water makes the water column stable. In fall and winter, strong northerly winds drive the light surface water westward, toward the Greenland shelf. This makes the water masses more unstable. As a result, the surface water sinks quickly when it is cooled and becomes denser.
"This transport of surface water is a requirement for deepwater formation", says Våge.
Natural and artificial submarines
Kjetil Våge and his colleagues are among the few who have measurement campaigns in this region during winter. Gathering data for their article, they got help from natural and artificial submarines – seals and gliders.
The gliders are drones of the sea, in this case resembling yellow vacuum cleaners with wings and tails. They can be remotely controlled to dive down into the deep and back up, and to glide exactly where you want measurements. During the winter of 2015–2016, the researchers let a glider glide back an forth in the ocean east of Greenland. Every time it came to the surface, it sent data to Bergen via satellite.
There was only one problem.
"We did not dare to send it too close to the ice edge", says Kjetil Våge.
In-between the ice floes and under the ice, a glider can easily hit something and damage itself. To keep it safe, data were collected to the east of the core of the southward flowing East Greenland current. There, the researchers observed that the water was cooled and that surface water was mixed more than 400 meters down into the ocean.
Data from instrumented seals, acquired by other research institutes, confirmed the results from the gliders.
Whether a similar degree of downwelling occurs farther west, in the core of the current, is still unknown. New ice-avoidance software allows the scientists to send the gliders closer to the ice edge this year. Hopefully, data from this measurement campaign will bring them closer to knowing how much the overturning off the coast of East Greenland means for the circulation in the Atlantic Ocean.
Read M.Sc. student Silje Skjelsvik's report from the cruise: Rough Seas and Northern Lights
Kjetil Våge, Lukas Papritz, Lisbeth Håvik, Michael A. Spall & G.W.K. Moore (2018): Ocean convection linked to the recent ice edge retreat along east Greenland. Nature Communications, 9. DOI: 10.1038/s41467-018-03468-6