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Modes a Sud-Committee — For illustrations of the application of the roots of C, Cernuschi, Brothers, Cerrone, Giuseppe, Cortani, Annibale. The appropriate mathematical bases and illustrations are included in the Cernuschi, Massimo; Smiraglia, Claudio; Diolaiuti, Guglielmina Adele.

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Ling Roth Wilhelm Dittmer. Louis Hutter Chrischta Ganz. The photo was taken by G. Diolaiuti from the summit of Mount San Matteo m, the white triangle in the map. A : Carte du glacier Forni. B : Photo du glacier Forni, prise par G. Diolaiuti depuis le sommet du Mont San Matteo m, le triangle blanc sur la carte. A: Map of the Val Viola glaciarised basin; 1: glacier area; 2: glacier area. Photo of the Val Viola glaciarised basin photo by G.

B : Photo du bassin glaciaire du Val Viola, par G. Matteo, at an elevation range between 3 m and 2 m a. The Forni Glacier has been visited for scientific and tourist purposes Stoppani, ; Smiraglia, a and b, , ; Guglielmin et al. Stoppani and published in the year The drawing of the Forni Glacier was made some years before the book publication and it was probably made in The Forni Glacier always represented a tourist attraction-pole and the homonymous hotel located at m a.

The Forni Glacier is also included in the list of glaciers monitored by the Italian Glaciological Committee to evaluate changes in length Comitato Glaciologico Italiano, , ; moreover from historic maps and aerial photos, its area coverage has been calculated for the last years. The results show that the Forni Glacier has experienced a marked decrease in length and area: from In the same time frame its tongue retreated by about 2 km fig.

A: photo by V. B: photo by A. C: photo by C. D: photo by C. A: photo V. B: photo A. C: photo C. D: photo C. Fluctuation data for the glacier terminus show a basic retreating trend from to the present. A more detailed analysis of the front fig. The retreat rates evaluated for recent decades tab. The Forni glacier was also the scene of an important event in Italian history during the First World War, when battles were fought on the glacier surface and on the mountain ridges overlooking the glacier valley.

These events and the remaining evidence, now revealed by the large quantity of ruins and finds present at the glacier surface, add a cultural value to the glacier. Total length variation in m. Presently thirty glaciers are located in the Val Viola glacierised basin, covering altogether an area of approximately 4 km 2 , with different shapes, sizes and morphologies. The Val Viola area boasts a long series of investigations evaluating glacier terminus fluctuations, beginning in the first half of the 20th century Comitato Glaciologico Italiano, , , mapping and dating the well preserved moraine ridges Diolaiuti, and evaluating glacier mass balance, ice thicknesses and volume by radio-echo-sounding surveys.

More recently, the area was studied to investigate the glacier micro-meteorology Diolaiuti et al. The comparison between the photographs shown in fig. This numerical increase is a direct consequence of the ongoing deglaciation phase, which causes the fragmentation of previous larger glaciers and generating newly formed smaller ones.

Further detail also enables in-depth analysis of length reduction in some selected glaciers located in the Val Viola basin. The terminus fluctuation trend fig. In order to evaluate glacier changes for the whole Val Viola glacierised basin over the last 50 years we analysed aerial photos dating from up to recent years. We compiled the , , and records by defining glacier outlines on aerial photographs , , and flights and importing them to a GIS environment.

The database, on the other hand, was compiled by previous authors Servizio Glaciologico Lombardo, Area km 2. Data were obtained by analysing aerial photos and and orthophotos , and by previous regional glacier inventory Servizio Glaciologico Lombardo, With grey colour were marked whose areas were evaluated and reported in four records , , and thus permitting the largest and more meaningful comparison.

The surface decrease resulted to be stronger in the last period time frame. So in order to evaluate the area changes we compared only the surface coverage of glaciers present in all the datasets glaciers shown in grey in tab. For this purpose we considered the , , and records, which enabled a comparison of the largest number of glaciers. The subset of glaciers analysed covered an area of 7. The area change between and was Moreover, the surface reduction seems to be stronger in the last time frame; in fact, the area change in the period 12 years was Furthermore, area changes in the Val Viola glaciers were analysed against total glacier areas fig.

The results showed that the smaller the glacier the faster the reduction in size, reflecting findings by other authors for different Alpine glacierised sectors Paul et al. All these studies underlined the scientific values of the Val Viola glacierised basin and the importance of its glaciers for the scientific community as witnesses of the ongoing climate change.

The economic and cultural values of the valley also supported its inclusion in the Lombardy Region Geosite List Regione Lombardia, It resulted the smaller glaciers to have experienced the stronger variations.

Le graphique montre que les glaciers les plus petits ont connu les variations les plus fortes. Another important landscape change is the increasing rock debris coverage. In fact, the Forni Glacier tongue, which has been always characterised only by two main medial moraines both Ice Stream Interaction and Ablation Dominant types, see Smiraglia, , now shows the increasing presence of supraglacial rock debris cover, ranging from quite continuous to sparse and sporadic; the surfaces of Val Viola glaciers also present increasing rock debris coverage fig.

In addition, glacier recession induced by climate warming causes an increase in supra-glacial slopes, enhancing the rate of paraglacially mobilised debris input, either from bedrock or pre-existing sediment storages on the glacier surface below. Consequently, the supra-glacial debris cover is prone to enlargement. When glacier fronts become partially inactive, little shear fractures can channel the englacial sediments to the surface, covering the frontal part of the glacier surface with debris, some times forming shear moraines.

The complexity of such phenomena explains the different debris cover distribution at the surface of the Forni Glacier and Val Viola Glaciers. Then the presence and the different distribution of supraglacial debris drive the genesis and the evolution of supraglacial morphologies due to differential ablation processes. On the Forni and the Val Viola glacier tongues fig. These morphologies are not exclusive to glacier recession but they are increasing in number and are becoming dominant in the epiglacial landscape due to the abundance of supraglacial debris following glacier shrinkage.

In addition, differential ablation processes also produce strong gravitational and meltwater reworking of the former debris covered surface. The flanks of dirt cones and of medial moraines gradually become steeper, the abundance of debris and water produces debris flows and sliding - processes that redistribute sediments on the glacier surface, change the pattern of differential ablation and create in the deglaciation phases very characteristic and distinctive features.

B : Glacier table on Forni Glacier surface. On the lower central sector of the Forni glacier tongue, at present almost continuously covered in debris, the larger ice losses are mainly concentrated at the debris free areas such as the walls of open crevasses and other holes on the glacier surface and steep marginal areas. Ablation proceeds by the preferential melting and retreat of such slopes, in a process known as backwasting Eyles, This process enlarges holes and produces a chain of a circular depression filled with water and favours the collapse of the roofs of englacial and subglacial water conduits Kirkbride, ; the process results in a sequence of landscapes similar to the evolution of karst features on limestone terrain and is thus defined as glacier karst Clayton, The ice cave developed from an abandoned sector of the glacier tongue.

The dead ice was covered by a thick debris layer which reduced ice ablation thus permitting it to survive. The ice cave ca. This morphology constituted an attractive feature for tourists and climbers thus contributing to increasing the popularity of the Val Viola basin.

All of these features - increasing in number on the Forni Glacier tongue and on the Val Viola glacier surface due to rising supraglacial debris coverage - are temporarily increasing local geodiversity. The debris-covered ice constituting the cave permitted it to survive and to be appreciable over the last three years.

It became an attraction for tourists and climbers photo by A. Elle est ainsi devenue une attraction pour les randonneurs et les alpinistes photo A. They are characterised by fast evolution and in the space of a few years they can cause glacier fragmentation.

On the Forni Glacier, several outcrops are evident on ice seracs connecting the three upper accumulation basins with the main ablation tongue. Here the steepness of the rock slopes drives ice-flow, thereby reducing ice thickness and shaping the flows as actual ice falls. In particular, on the east ice fall an outcrop has been developing over the last three years. This outcrop is causing a separation between the upper east accumulation basin and the main glacier tongue fig.

The eventual result of this evolution will be the transformation of the east accumulation basin into an isolated cirque glacier. The newly formed lakes are located at the glacier surface, at the glacier boundary lateral and frontal position and in the glacier forefield. The lakes located at the Forni Glacier surface are actually large water ponds which act as heat-storage, thus increasing surface melting and accelerating glacier recession.

Their evolution is fast and generally their lifespan is shorter than one year. The lakes located at the glacier boundary are the ice—contact type fig. These are becoming increasingly widespread morphologies, not only at the Forni Glacier boundary but also at the contact of several Alpine glaciers due to the current phase of glacier shrinkage.

In fact, the retreat of glacier termini has produced favourable settings for ponding of small ice-contact lakes behind moraine ridges, particularly those formed by the most recent glacier advance in the late 20th century, or in less frequent cases e. The ice-contact conditions allow calving phenomena to occur, driving generation of icebergs. At the Forni Glacier calving events are limited and they occur on a smaller scale compared with glacier calving found at higher latitudes, nevertheless the phenomenon exists and is appreciable.

The lifespan of ice-water contact at alpine glaciers is, however, generally limited. Either most of the newly formed lakes disappear after a few years, or the accelerating retreat of the glacier snouts implies a rapid evolution from ice-contact to distal proglacial lakes Masetti et al. The persistence in time and space of such conditions seems to be longer where the glacier surface in the ice-contact zone is covered by debris that reduces ablation i.

B: Ice contact lake at the lateral side of Forni Glacier in , it is appreciable the debris-covered glacier ice constituting the lake dam. The ice-core of the lateral moraine is visible as well. The Forni Glacier ice contact lake is now experiencing a growing phase and during the last 4 years it passed from being a simple small water pond, to its present maximum length exceeding m.

Furthermore, lateral moraines too are experiencing deep changes due to ongoing climate change. This is the case of the lateral moraines of the Forni Glacier, affected by ice core melting with subsequent collapse and genesis of mud and debris flows. The moraine ridges providing evidence of such events were deposited by the glacier during the last advancing phase seventies-eighties of the 20th century, see fig.

In fact, starting from the nineties, several phenomena of fast slope evolution, due to ice core melting, occurred mainly mud and debris flow events , causing radical changes in moraine morphology and prompting a modification of the tourist-trail enabling access to the glacier snout Smiraglia et al.

The consequences of this rapid evolution for geosite assessment, management, conservation and valorisation are important and demand urgent strategies to manage such zones, which represent a unique tool for raising public awareness of climate change impact. On the other hand such territories are fragile due to the rapid variations they are undergoing, requiring guided visits to prevent accelerated degradation of morphological evidence.

In addition, the analysis of regional glacier inventories we performed together with the studies carried out at a local scale i. The glacial reduction demonstrated by these findings is interpreted as a real impact of climate change. Indeed, as the transfer function between climate changes and glacier variations does not change in time Oerlemans, , an acceleration in glacial changes is suggested. Extrapolations of developments documented by repeated glacier inventories Kaab et al.

The Forni Glacier and Val Viola basin glaciers could also be victims of this ominous scenario if no meaningful changes occur in the climate warming trend. The Forni Glacier will firstly be split into three smaller glaciers due to fragmentation of the present glacier body, then the newly formed cirque glaciers will dwindle and will have completely vanished by the end of this century.

In the case of the Val Viola basin, the glacier decline and disappearance will be faster and may occur and be completed within the next two decades. These ongoing shrinkage phenomena are changing in a radical way the mountain landscape of the Lombardy Alps.

Furthermore, the retreat and extinction of mountain glaciers and the disappearance of the geomorphosites linked to their presence are occurring together with the genesis of new, smaller geomorphosites, which in turn trigger a new complex landscape system. The morphologies described above, found at the surface and at the boundary of the Forni and Val Viola glaciers, are good examples of such phenomenon. From a geodynamical point of view, the transition is now taking place from a glacial system to a paraglacial one sensu Ballantyne and Benn, , ; Curry and Ballantyne, Areas where in the recent past the main shaping and driving factors were glaciers are now subject to the action of melting water, slope evolution and dynamics and periglacial processes.

The next step will be the transition from a paraglacial environment, where ice-patches or glacierets are presents, to a periglacial environment where cold and snow are dominant, without ice glaciers or ice melt water. This is particularly true considering the changes affecting the Forni Glacier, where the present retreat of the glacier snout is generating an ice-free, wide and quite flat area which promotes deposition processes and building of fresh morphologies.

Furthermore, when the Forni Glacier and the Val Viola glaciers have completely disappeared, a major visible impact will occur in the aesthetic value of the mountains. Ice melting will turn the snow-covered mountains into bare, rocky mountains. The dynamic glaciers will turn into lifeless rubble without their icy core.

And in addition to these changes impacting on tourism and culture, the lack of snow and ice will also have consequences on the climbing experience. Some scientists show optimistic prospects based on the possibility that vegetation and plants will rapidly colonise the deglaciated areas. This is an ongoing process on the upper deglaciated sectors see our photo comparisons in fig. In reality, several authors and our findings suggest the developments of the next decades will include the complete disappearance of small mountain glaciers and down wasting , rather than retreat for long valley glaciers Haeberli, This already discernable trend may be accompanied by the development of extreme and long-lasting disequilibria in the abiotic as well as the biotic parts of ecosystems and habitats, not only in high mountain areas but elsewhere Watson and Haeberli, In this context attention must be paid to the question of conservation.

The action needed to safeguard glacier heritage includes:. In particular, regarding mitigation strategies some attempts have been made to reduce ice and snow melting by applying artificial coverage preventive action, see Olefs and Fisher, , and on the Val Viola Basin, Diolaiuti et al. In this field the greatest efforts made include adaptation of tourist glacier trails e.

In this field a lot could be done to increase awareness of climate change and human responsibilities, and to prepare people for the eventuality of a possible future alpine landscape without glaciers cultural adaptation strategies. Then our once beautiful glacierised mountains, such as the Forni Valley and Val Viola Basin, are now deeply changing, becoming key witnesses to the general and serious impact humans have wrought on the Planet Watson and Haeberli, In this sense glacier monitoring programmes are becoming activities of ever increasing socio-economic and political importance Haeberli, and projects for promotion and conservation of glacier geosites may give people the chance to raise their awareness of global environmental change.

Anderson R. Journal of Glaciology 46, Ballantyne C. Arctic and Alpine Research 25, In Anderson M. Wiley, Chichester, Barla G. Landslide News 13, Beniston M. Arnold, London, p. Climatic Change 59, Benn D. Oxford University Press, Oxford, p. Biancotti A. Bollettino Geofisico , International Journal of Climatology 21, Buzzini, B. Turchetti, G. Diolaiuti, C. Martini, C. Smiraglia — Yeast biodiversity in melting ice from glaciers in the Italian Alps. Annals of Glaciology 40, Cayla N.

Edytem , 8, Casty C. International Journal of Climatolology 25, Chiarle M. Global and Planetary Change 56, Citterio M. Geografia Fisica e Dinamica Quaternaria , 30, Clayton L. Journal of Glaciology 5, Comitato Glaciologico Italiano — Campagne Glaciologiche.

Geografia Fisica e Dinamica Quaternaria Cook A. Science , Curry A. Deline P. The Holocene 15, Quaternary Science Reviews , in press doi Geografia Fisica e Dinamica Quaternaria 27, Diolaiuti G. In Bernardi R. Geotema 14, Cold Regions Science and Technology 44, Prime applicazioni italiane e risultati. Neve e Valanghe 65, In Smiraglia C. La crisi delle risorse glaciali in Lombardia.

Regione Lombardia, Milano, Dyurgerov M. Proceedings of the National Academy of Sciences 97, Eberhard R. Elsasser H. Mountain Research and Development 21, Erikstad L. In Barettino D. Evans S. Geomorphology 10, Eyles N. Canadian Journal of Earth Sciences 16, Ferrarini A. Biological Conservation , The Holocene 18, Gray M. Wiley, Chichester, p. Gruber S. Related destabilization following climate change.

Journal of Geophysical Research , F02S18 doi Guglielmin M. Misurazioni tramite Sondaggi Elettrici Verticali. Neve e Valanghe 24, Haeberli W. In Orlove B.

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Indexing variable names matlab torrent Preethaji Krishnaji. Cima Dugorale. Panizza M. The persistence in time and space of such conditions seems to be longer where the glacier surface in the ice-contact zone is covered by debris that reduces ablation i. Cristina M. In Piacente S. Bergamo, Bolis, p.
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The ring 2002 movie download utorrent Ami Claudio cernuschi illustrator torrent Anthony David. These glacier geomorphosites represent well the variations affecting all Alpine glaciers ; these variations are not only driving significant changes in the morphology and ecology of the present mountain landscape, but at the same time are shaping newly formed morphologies, which may develop into smaller geomorphosites with significant value from a scientific and cultural point of view. B: photo A. Natural systems will not be the only victims of glacier recession: the economies of mountain areas will also be affected. Annals of Glaciology 43,
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