Glaciers of the Adamello-Presanella Group (Central Alps, Italy): areal and volume reductions since the Little Ice Age.
María Cristina Salvatore, Carlo Davide Baroni, Alberto Carton
Abstract
María Cristina Salvatore, Carlo Davide Baroni, Alberto Carton
Abstract
More than one hundred glaciers (including the widest glacier of the Italian Alps, the Ghiacciaio\ndell'Adamello) are presently extended about 53 km2. As documented in other alpine sectors\nand in several other regions, glaciers of the Adamello-Presanella Group (Central Alps,\nItaly) reached their maximum Holocene extension during the Little Ice Age (LIA). LIA glaciers\nlimits have been reconstructed on the basis of geomorphologic and glacial geologic field\nsurveys and mapped at the scale of 1:10,000. More recent (XXth Century) glacier limits have\nbeen detected from historical maps and multitemporal aerial photographs.\nAll the collected data have been georeferenced (photographic documents using a direct linear\ntransformation to correct tilting and relief displacement) and managed using a GIS for evaluating\nthe most relevant quantitative parameters. In particular, glacier area loss and volume\nreduction have been determined. More than 140 glaciers developed during the LIA covering\nan area almost the double of their present surface. Since the middle of the XIX Century there\nhas been a vigorous reduction in thickness and area extension of glacier bodies, broken by\nbrief and weak advances. The notable regression of the fronts is marked by withdrawals ranging\nfrom several hundred meters to more than 2000 m. About 90 of LIA glaciers (extended\nabout 8 km2) are presently extinguished. The apparent conflicting numbers of LIA and active\nglaciers (140 LIA glaciers - 90 extinguished = 101 active glaciers!) can be explained considering\nthe fragmentation of LIA glacial bodies induced by their retreat.\nBetween the maximum LIA extension and 1983 AD, glaciers of the Presanella Group lost\nabout 55% of the total area while the mean value for the entire Adamello- Presanella Group is\nabout 50%.\nAn additional reduction of about 25% occurred between 1983 and 1999 AD, of which about\n15% between 1983 -1994 and about 10% between 1994 and 1995. Preliminary data on volumetric\nvariations show that the glaciers of the Adamello-Presanella Group lost about 30\nm3/m2 between 1850 and 1983 AD.\nArea loss and volumetric variations supply new data for reconstructing the environmental\nevolution and climatic history of the Central Italian Alps. The glacier retreat scenario gives us\nthe possibility for better understanding glaciers dynamics and their behaviour in reacting to\nglobal environmental changes. Moreover, the enduring process of glacier retreat and ice melting\nin alpine environments enhances the risk of natural hazards. Finally, considering the great amount of water stored in alpine glaciers (easily available and\nsubstantially uncontaminated, this research is of particular interest\n(1) for estimating the amount of ice melting as a consequence of global warming,\n(2) for modelling future availability of melt-water, and\n(3) for better planning the correct management of water as natural resource.
A significance statement is not available in the OpenAlex record.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
More than one hundred glaciers (including the widest glacier of the Italian Alps, the Ghiacciaio\ndell'Adamello) are presently extended about 53 km2. As documented in other alpine sectors\nand in several other regions, glaciers of the Adamello-Presanella Group (Central Alps,\nItaly) reached their maximum Holocene extension during the Little Ice Age (LIA). LIA glaciers\nlimits have been reconstructed on the basis of geomorphologic and glacial geologic field\nsurveys and mapped at the scale of 1:10,000. More recent (XXth Century) glacier limits have\nbeen detected from historical maps and multitemporal aerial photographs.\nAll the collected data have been georeferenced (photographic documents using a direct linear\ntransformation to correct tilting and relief displacement) and managed using a GIS for evaluating\nthe most relevant quantitative parameters. In particular, glacier area loss and volume\nreduction have been determined. More than 140 glaciers developed during the LIA covering\nan area almost the double of their present surface. Since the middle of the XIX Century there\nhas been a vigorous reduction in thickness and area extension of glacier bodies, broken by\nbrief and weak advances. The notable regression of the fronts is marked by withdrawals ranging\nfrom several hundred meters to more than 2000 m. About 90 of LIA glaciers (extended\nabout 8 km2) are presently extinguished. The apparent conflicting numbers of LIA and active\nglaciers (140 LIA glaciers - 90 extinguished = 101 active glaciers!) can be explained considering\nthe fragmentation of LIA glacial bodies induced by their retreat.\nBetween the maximum LIA extension and 1983 AD, glaciers of the Presanella Group lost\nabout 55% of the total area while the mean value for the entire Adamello- Presanella Group is\nabout 50%.\nAn additional reduction of about 25% occurred between 1983 and 1999 AD, of which about\n15% between 1983 -1994 and about 10% between 1994 and 1995. Preliminary data on volumetric\nvariations show that the glaciers of the Adamello-Presanella Group lost about 30\nm3/m2 between 1850 and 1983 AD.\nArea loss and volumetric variations supply new data for reconstructing the environmental\nevolution and climatic history of the Central Italian Alps. The glacier retreat scenario gives us\nthe possibility for better understanding glaciers dynamics and their behaviour in reacting to\nglobal environmental changes. Moreover, the enduring process of glacier retreat and ice melting\nin alpine environments enhances the risk of natural hazards. Finally, considering the great amount of water stored in alpine glaciers (easily available and\nsubstantially uncontaminated, this research is of particular interest\n(1) for estimating the amount of ice melting as a consequence of global warming,\n(2) for modelling future availability of melt-water, and\n(3) for better planning the correct management of water as natural resource.
Key concepts: Glacier, Geology, Glacier morphology, Little ice age, Physical geography, Ice caps, Geomorphology, Geography