Press release

Italian alpine glacier now accelerating after 7000 years


The Mt Ortles (3905 m) in South Tyrol from which were extracted in 2011 the ice cores
The Mt Ortles (3905 m) in South Tyrol from which were extracted in 2011 the ice cores

An international study, in which the Istituto per la dinamica dei processi ambientali of Consiglio nazionale delle ricerche (Idpa-Cnr) was involved, and which was published in The Cryosphere, found that the deepest and oldest ice from Mt. Ortles (3905 m, South Tyrol, Italy) started to move for the first time since the period of the famous Tyrolean Iceman. The first Alpine ice cores drilled to bedrock in an Eastern Alps glacier, only 37 km from where the Tyrolean Iceman was discovered, suggest that the flow of the highest glacier of South Tyrol is now accelerating and that this is unprecedented in 7000 years. Evidence comes from deep ice core sections, dated by using the carbon 14 technique, and from the glacial borehole, equipped with an inclinometer, a very sensitive instrument that can detect very small movements down to great glacier depth. "These cores offer the unique opportunity to study the atmospheric content when the Tyrolean Iceman was living in this region, offering the possibility to better understand the environment and the climate that he experienced" says Prof. Carlo Barbante, Director of Idpa-Cnr, Venice.

The rapid retreat of glaciers is linked to global warming. “Glaciers in the Alps are rapidly retreating due to intense melting caused by the recent atmospheric warming” said project leader Dr. Paolo Gabrielli, research scientist at Byrd Polar and Climate Research Center of The Ohio State University in the USA. “Our results indicate that a previously unrecognized process might accelerate the flow of Alpine glaciers even at high elevation, perhaps contributing to speed their shrinking”.

Also of particular interest to the researchers is the possibility to obtain information about modern climatic changes. “The Ortles ice cores offer the unique possibility to closely verify if and how regional environmental changes can interact with climatic changes of global significance” Dr. Gabrielli says. For example, among the other signals preserved in the ice, the researchers have already detected the low but distinct signal of the radioactive fallout from the Fukushima nuclear power plant accident that occurred in Japan during March 2011, a few months earlier than the drilling operation.

“It is possible that some meltwater infiltrated in depth from the rock outcrops uphill of the drilling site and it is now lubricating the glacier base during the current exceptionally warm summers, thus facilitating the basal ice sliding” continues Gabrielli.

The results of this research indicate that the Mt. Ortles glacier, as we know it today, formed 7000 years ago, at the end of the so-called “Northern Hemisphere Climatic Optimum”, a particularly warm period when glaciers in the Alps retreated to high elevations. Successively, the onset of a cooler period contributed to the accumulation of snow and ice on the renewed frozen bedrock atop Mt. Ortles. This new climatic period, called Neoglaciation, also contributed to burying and preserving the mummy of the Tyrolean Iceman until the end of summer 1991, when he emerged from the ablating ice of the nearby glacier saddle of the Tisenjoch, at 3210 meters elevation. The researchers are also beginning to analyze the ice cores they drilled. The isotopes of oxygen, major ions, black carbon, pollen, trace metals and dust sealed in the ice will give detailed clues to the climatic conditions since the ice was formed 7000 years ago. “One of the ice cores extracted may be part of the Ice Memory Project, a new international program that aims to transport ice cores from mid-latitude regions to a repository in Antarctica in order to safeguard these precious glacial archives for future generations of scientists” concludes Prof. Barbante, Director of Idpa-Cnr.

The ice cores were drilled by an international team of glaciologists led by The Ohio State University, with the logistic support of the Autonomous Province of Bolzano, and the active involvement of researchers of Idpa-Cnr. International collaborators hailed from the The Ohio State University and the U.S. Geological Survey in the USA; the University of Venice, Istituto per la Dinamica dei Processi Ambientali-Cnr, University of Padova, University of Udine, Provincia Autonoma di Bolzano, Geologin, ENEA, Waterstones Geomonitoring, the University of Pavia all of Italy; the Central Institute for Meteorology and Geodynamics ZAMG and the University of Innsbruck in Austria, Laboratoire de Glaciologie et Géophysique de l’Environnement (LGGE), CNRS and the University Grenoble Alpes in France; the Paul Scherrer Institut and the University of Bern in Switzerland; and the Russian Academy of Sciences in Russia. This work was funded by the National Science Foundation in the USA and by the Autonomous Province of Bolzano in Italy.

Roma, January 30, 2017

In summary

Who: the Istituto per la dinamica dei processi ambientali of Cnr (Idpa-Cnr).

What: the study of the age and the flow of the Mt. Ortles Glacier, “Age of the Mt. Ortles ice cores, the Tyrolean Iceman and glaciation of the highest summit of South Tyrol since the Northern Hemisphere Climatic Optimum” published in The Cryosphere, 10, 2779–2797, 2016. Gabrielli, P., Barbante, C., Bertagna, G., Bertó, M., Binder, D., Carton, A., Carturan, L., Cazorzi, F., Cozzi, G., Dalla Fontana, G., Davis, M., De Blasi, F., Dinale, R., Dragà, G., Dreossi, G., Festi, D., Frezzotti, M., Gabrieli, J., Galos, S., Ginot, P., Heidenwolf, P., Jenk, T. M., Kehrwald, N., Kenny, D., Magand, O., Mair, V., Mikhalenko, V. N., Lin, P. N., Oeggl, K., Piffer, G., Rinaldi, M., Schotterer, U., Schwikowski, M., Seppi, R., Spolaor, A., Stenni, B., Tonidandel, D., Uglietti, C., Zagorodnov, V. S., Zanoner, T., and Zennaro, P.

Per informazioni:
Carlo Barbante
Contact in USA
Paolo Gabrielli, e-mail:
tel. +001.(614)292-6664

Ufficio stampa:
Emanuele Guerrini
Ufficio stampa Cnr

Capo ufficio stampa:
Marco Ferrazzoli
06 4993 3383
skype marco.ferrazzoli1

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