An international scientific expedition recently completed a complex drilling operation at the Crary Ice Rise sitea remote camp located 700 kilometers from New Zealand’s Scott Base in the Ross Sea. The undertaking, conducted in extreme environmental conditions, made it possible to exceed the initial objectives by reaching a depth of 228 meters, penetrating geological sediments dating back millions of years. The operation is part of the SWAIS2C (Sensitivity of the West Antarctic Ice Sheet to 2°C) project, a collaboration involving researchers, engineers and drillers from ten nations, including Italy, the United States, New Zealand and the United Kingdom.
The objective: to monitor the +2°C threshold
The focus of the research lies in understanding the vulnerability of the Ross Shelf (the largest mass of floating ice in the world) and the West Antarctic Ice Sheet (WAIS). Scientists mean determine whether an increase in global average temperature of +2°C compared to the pre-industrial era could trigger irreversible melting.
The stability of the WAIS is strictly dependent on the stability of the Ross Platform: its failure would cause a chain melting of the continental ice cap, with a potential rise in global sea levels estimated at between 4 and 5 metres.
Below is the animation of the operation
The role of Italian research
Italy plays a leading role in the project through a network of academic and institutional excellence. THE’National Institute of Geophysics and Volcanology (INGV) leads national governance, collaborating with theNational Institute of Oceanography and Experimental Geophysics (OGS) and the Universities of Siena, Trieste and Genoa.
“The National Institute of Geophysics and Volcanology (INGV) is at the forefront in the governance of SWAIS2C as regards Italy“, clarifies the President of INGV Fabio Florindo. “Furthermore, staff from the Institute participate in the scientific part of the study of the ice core recovered from the Crary Ice Rise by making their skills in chronostratigraphy, volcanology, petrology and paleomagnetism available to the team of over 120 scientists“.
Towards the definition of the “Point of no return”
The project, funded by the International Continental Drilling Program (ICDP), aims to provide direct geological evidence of the so-called tipping point. The study of ice cores and extracted sediments will allow us to reconstruct the climatic variations of the remote past, offering fundamental data for developing projections on the future evolution of our planet. The ability to identify the moment in which melting becomes irreversible represents one of the most urgent scientific challenges for the protection of global coastal zones today..
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