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Suretta Sud Glacier - Servizio Glaciologico Lombardo

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2008 glaciological<br />

Survey<br />

moraine cover, the frequent dismemberments<br />

induced by the loss of mass (Passo<br />

di Chiareggio, Venerocolo, Porola), the formation<br />

and widening of proglacial lakes (particularly<br />

important is the widening of the Est<br />

Fellaria proglacial lake) and the lessening of<br />

break-up morphologies (crevasses, seracs).<br />

Hence, briefly, the negative trend for our<br />

The data of the 2008 Survey<br />

Year<br />

Total regional area covered<br />

by glaciers (ha)<br />

- 24 -<br />

glaciers continued in 2008 as well, though<br />

we could say something like “better than<br />

worse”. Coming from years that were anticipating<br />

the glaciological and climatic scenarios<br />

predicted for the end of XXI century,<br />

this might be of some satisfaction.<br />

During the 2008 Glaciological Survey, 96 glaciers were subjected to a complete glaciological<br />

survey 1 (36,5% of existing glaciers); their combined area was 9061,4 ha or 83,6% of Lombardy<br />

glacialized surface. Adding the photographic observations2 (103) the number of glacial apparatuses,<br />

inclusive of both glaciers and glacierettes, increases to 199 (75,7 % of all glacial bodies<br />

or 95,4 % of the entire regional glacial area).<br />

Tab. 1: total glacialized regional surface investigated during the 2008 Glaciological Survey and comparisons<br />

with the previous biennium (absolute values in ha and %) (* without photographic observations).<br />

Total area investigated<br />

(ha)<br />

Total area surveyed (%)<br />

2006 11.004,7 8.690,0 79*<br />

2007 10.967,7 10.242,8 93,3<br />

2008 10.838,6 10.344,1 95,4<br />

1 Complete glaciological survey means that a detailed on-site investigation was performed by the designated<br />

operators; where possible, their evaluation included: snow line altitude, minimum altitude of the front, front<br />

measurements. Operators also remarked the morphologies variations versus the previous survey.<br />

2 Photographic observation means that a glacier is investigated through one or more photos taken from<br />

selected photographic stations to allow meaningful comparisons over the years. Such observations do not<br />

provide dynamic indexes.

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