Breathing space for the Gulf Stream

Using a newly developed computer model, an international team of scientists led by the GEOMAR Helmholtz Centre for Ocean Research Kiel has now simulated in detail the pathways and effects of the additional meltwater. "The effects of the melting Greenland glaciers initially remain smaller than expected, since a large part of the meltwater is effectively flushed out by fast, narrow currents along the coastline of North America. Thus changes in the critical, northern seas are delayed," explains GEOMAR researcher Prof. Claus Böning, lead author of the study.

The computer model takes into account the regional differences in meltwater discharge trends and very fine details of the ocean currents. This fine detail allowed the researchers to assess more accurately the influences of the narrow boundary currents and small-scale eddies on the water exchange between the coastal shelf and the deep ocean.

The model calculations showed that more than half of the meltwater is transported southwards along the Canadian coast by the Labrador Current. Less than 20 percent remain in the area between Greenland and Labrador which is critical for the Gulf Stream system. The model suggests that the melting-induced impact on ocean salinity is, to date, only half as large as natural variations measured in the past decades.

However, the simulation also shows a progressive trend in the freshening of the Labrador Sea. "If we project the rise in Greenland melting rates into the future, we expect first noticeable changes in the Labrador Sea in two or three decades," emphasizes Professor Böning, "in this sense the Gulf Stream may just get some breathing space." "Meltwater fluxes from Greenland have been accelerating in recent years and if, as seems likely, this trend continues we could see changes in ocean circulation even sooner" explains co-author Jonathan Bamber, Professor at the University of Bristol.