Australasian Science: Australia's authority on science since 1938

Roaring Cave Reveals How Climate Changed History

Research led by UNSW Australia has produced a 3000-year-long record of climatic variations that may have influenced historical events such as the fall of the Roman Empire and the Viking Age of expansion.

The study of five stalagmites in Roaring Cave in north-west Scotland is the first to use a compilation of cave measurements to track changes in a climate phenomenon called the North Atlantic Oscillation.

“Our results also provide the longest annual record of this important phenomenon, which has a big impact on the climate in Europe,” says Prof Andy Baker. “It confirms that during the Medieval Warm Period, between 1080 and 1430, the oscillation index was in an un­usually prolonged positive phase, which brings increased rain to Scotland and drier conditions in the western Mediterranean.

“Our results also reveal there was another persistent positive phase between 290 and 550, which coincides with the decline of Rome and a period of intensified human migration in southern Europe during the Dark Ages.

“This was followed by a persistent negative phase between 600 and 900, which may have provided warm and dry conditions in north-western Europe that made it suitable for westward expansion by the Vikings, although the precise timing of this event is contested.”

The North Atlantic Oscillation climate index measures the air pressure difference between Iceland and the Azores islands off the Portuguese coast, and is a record of the strength of the westerly winds in the North Atlantic.

Rainfall levels in this region closely correspond with the strength of the oscillation index in winter, with higher precipitation when it is positive. The upward rate of growth of stalagmites in the cave is very sensitive to rainfall – the more water in the peat deposited above the cave over thousands of years, the more slowly the stalagmites grow.

“We painstakingly measured the thickness of each annual growth ring in five stalagmites taken from the cave, including one

that provides a continuous annual record spanning more than 1800 years,” Baker says. By overlapping the five stalagmites they obtained a proxy record of the climate at the cave during a 3000-year period from about 1000 BC to 2000 AD.

“Our research provides a climate context for some of the big human migration events in Europe, and allows us to start building hypotheses about the impact of environment on societal change,” Baker says.

The study has been published in Scientific Reports.