Retreating glacier ice will eventually open a new strait between the Barents and Greenland Seas through the island of Spitsbergen, the largest in the Norwegian Arctic archipelago of Svalbard.
That finding comes from radar soundings made by Polish researchers in the area of Hornbreen-Hambergbreen glacier system show that there are no obstacles that would hinder the flow of water through the channel.
Svalbard, the fastest-heating place on earth, is a live laboratory for everyone studying the dramatic effects of the climate crisis. While world leaders travels to New York on Sept. 23 for the U.N. Climate Action Summit to find ways to limit the global temperature to 1.5 degrees Celsius above pre-industrial levels, temperatures on Svalbard have already risen by 4 degrees C.
At Spitsbergen, the largest island on the archipelago, both permafrost and glacier are melting in a speed nobody could predict a few years ago.
Since 1957, Poland has operated a research station at Hornsund, the southernmost fjord on Spitsbergen. Researchers here are witnessing the melting Arctic firsthand. Although protected by law, no other nature park of such size in the world is changing more dramatically than Sør-Spitsbergen National Park.
“The conclusion coming from the surveys is that the glacier bed is below sea level and no obstacles have been identified that might prevent connection of the Barents Sea and Greenland Sea when glaciers have retreated,” Mariusz Grabiec told the Barents Observer.
Grabiec is a researcher with the University of Silesia and the Polish Centre for Polar Studies. He says that the fjord of Hornsund is expanding about 3 square kilometers every year as the glaciers melt away.
Named Hornsundbreen on the west side, the glacier is connected with the Hambergbreen on the east side towards the Barents Sea.
Grabiec has for the last 20 years studied glaciers on Svalbard and is deeply concerned about what he now sees.
“In southern Spitsbergen the retreat in the 21st century accelerate three times in comparison to the first part of the 20th century average rate.”
The team of researchers of the University of Silesia made radar soundings over a distance of 40 kilometers in two spring expeditions in 2013 and 2014 over the Hornbreen-Hambergbreen system allowing them to see the glacier depth and subglacial topography.
Reading the radar soundings, the team concluded that the land actually consists of two islands; Spitsbergen to the north and Sørkapp Land to the south.
“Based on the last few decades of glacier retreat rate, we estimated that the strait opening might happen sometime between 2055 and 2065,” Mariusz Grabiec tells.
Though, it might happen even faster.
“Having in mind the deglaciation rate in this area is getting faster, the glacier may disappear earlier.”
The front of Hornbreen has retreated by more than 14 kilometers since the end of the 19th century. The distance between Hornsund and the Barents Sea on the east side is now less than 6 kilometers.
Eventually, the southern part of Spitsbergen will become separated and will thus form the fourth largest island on the Svalbard archipelago. Sørkapp Land (South Cape Land) is 1,260 square kilometers.
The Polish researchers say the ambiguity inherent in the word ‘sound’ is therefore becoming very fitting for Hornsund — a fjord which is gradually becoming a strait.
Changing Arctic geography is not unique to Svalbard.
In the period 2015-2018, Russian navy researchers discovered more than 30 islands, bays, apes and straits at Novaya Zemlya and Franz Josef Land. The latest in August this year when five new islands separated from others at Franz Josef Land. The biggest was 54 square kilometers, the Barents Observer reported.
Norwegian broadcasting NRK recently reported on a new 10 square kilometer island separating from Nordaustlandet further north on Svalbard. What previously was believed to be a peninsula, suddenly became an island as the glacier melted, researchers at the Norwegian Polar Institute discovered after studying satellite images of the area from this summer.