Large dome of fresh water detected in Arctic Ocean
London: With the help of ESA satellites, scientists have discovered that a large dome of fresh water has been building up in the Arctic Ocean over the last 15 years.
A change in wind direction could cause the water to spill into the north Atlantic, cooling Europe.
The results are remarkable: since 2002, the sea surface in the studied area has risen by about 15 cm, and the volume of fresh water has increased by some 8000 cubic km – around 10percent of all the fresh water in the Arctic Ocean.
Researchers from the Centre for Polar Observation and Modelling (CPOM) at University College London and the UK’s National Oceanography Centre used data from ESA’s ERS-2 and Envisat satellites to measure sea-surface height over the western Arctic from 1995 to 2010.
The scientists concluded that the dome could be a result of strong Arctic winds accelerating a large ocean circulation known as the Beaufort Gyre, causing the sea surface to bulge.
A change in the direction of the wind would cause the fresh water to spill into the rest of the Arctic Ocean and even reach the north Atlantic.
This could slow a key ocean current, stemming from the Gulf Stream, and subsequently cool Europe.
This current keeps the continent relatively mild compared to other areas at similar latitudes.
“When we looked at our data on a year-to-year basis, we noticed that the changes in the sea surface height did not always follow what the wind was doing, so we thought about reasons why this might happen,” said Katharine Giles, CPOM research fellow and lead author of the study.
“One idea is that sea ice forms a barrier between the atmosphere and the ocean. So as the sea ice cover changes, the effect of the wind on the ocean might also change.
“Our next step is to look into how changes in the sea ice cover might affect the coupling between the atmosphere and the ocean in more detail to see if we can confirm this idea,” she stated.
The results were published yesterday in the online version of the scientific journal, Nature Geoscience.