“I would expect to see continuous permafrost start to thaw along the boundaries at this threshold of 1.5C [in future],” said Anton Vaks, of the Earth sciences department at Oxford, who led the research. Temperatures in the region were 0.5-1C higher than in modern times for a period about 120,000 years ago, and at that time stalactites in caves further south, near Lake Baikal, showed signs of growth, and therefore melting.
But for the same period, the stalactites in the far northern cave – called the Ledyanaya Lenskaya cave, near the town of Lensk at latitude 60N – did not grow, showing that the permafrost remained intact at those temperatures. “This indicates that 1.5C appears to be something of a tipping point,” said Vaks.
At present, global average temperatures are about 0.6C-0.7C above pre-industrial levels. This means, according to Vaks, that climate modellers should include the possibility of permafrost beginning to melt in their models.
The team of scientists, from Mongolia, Russia and Switzerland as well as the UK, used radiometric dating techniques on the cave formations. They report on their work in the journal Science Express, published on Thursday.
Vaks said the findings could have severe implications for the region, as melting permafrost could affect natural gas exploration and pipelines, as well as other infrastructure. It could also have more wide-reaching effects. “Although it wasn’t the main focus of our research, our work also suggest that in a world 1.5C warmer – warm enough to melt the coldest permafrost – adjoining regions would see significant changes. Mongolia’s Gobi Desert [could] become much wetter than it is today and this extremely arid area could come to resemble the present-day Asian steppes.”
He said more research was needed to establish the likely speed and scale of melting as temperatures rise.