Suretta Sud Glacier - Servizio Glaciologico Lombardo
Suretta Sud Glacier - Servizio Glaciologico Lombardo
Suretta Sud Glacier - Servizio Glaciologico Lombardo
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snow-meteo report<br />
A summary of the events<br />
The 2007-2008 Hydrological Year in the Italian Central Alps can be summarized as follows:<br />
•<br />
•<br />
•<br />
•<br />
Another negative autumn season for snow accumulations;<br />
A moist and snowy spring;<br />
A strong ablation in June, July and August;<br />
A cold and snowy September, marking the anticipated end of the ablation season.<br />
Accumulation season (1st October, 2007 – 30th June, 2008)<br />
The 2007-2008 accumulation season resulted,<br />
as it has often happened in the past few years,<br />
very unfavourable for the Lombardy glaciers.<br />
The abundant spring precipitations were<br />
not sufficient to grant a good supply to our<br />
glaciers: the many, large avalanches that<br />
followed April and May snowfalls have restocked<br />
only the few apparatuses fed by avalanches,<br />
while the same snow, characterized<br />
by a scanty resistance for lack of a proper<br />
compaction, did not help the other glaciers.<br />
Snow accumulations were very moderate in<br />
October, December and February; on the oth-<br />
Weather Station<br />
Precipitations in mm<br />
October, 2007 - June, 2008<br />
(Deviations from the mean<br />
value)<br />
- 8 -<br />
er side November snowfalls were scourged<br />
by strong northern currents that redistributed<br />
and eroded the snow on the ground.<br />
Though January was double-faced, the month<br />
can be judged positive for our glaciers. At<br />
first, moist Atlantic perturbations led to several<br />
episodes of abundant accumulations<br />
while in the second half of the month, good<br />
weather conditions and temperatures exceeding<br />
the average for the period had the positive<br />
effect of slowing down the constructive<br />
metamorphism process of the snow cover.<br />
March was also windy; as a conse-<br />
Tab. 1: Precipitation and temperature values during the 2007/2008 accumulation season. In order<br />
to allow a homogeneous comparison among the different stations, the mean value has been<br />
calculated for the period 1988/89 – 2005/06. “Integral” means that the average temperature has<br />
been calculated by adding each recorded value (data acquisition interval: 5’) and dividing the total<br />
by the number of readings. The other temperatures have been calculated with the “arithmetic”<br />
method: i.e. (average of daily maximum temperatures + average of daily minimum temperatures) / 2.<br />
Temperatures in °C<br />
October, 2007 - June, 2008<br />
(Deviations from the mean<br />
value)<br />
Passo Venerocolo - 3230 m/s.l.m. - - 6,7° (integrale - 7,0°) *<br />
Bivacco Corti - 2509 m/s.l.m. - - 0,4° (integrale - 1,7°)<br />
Bivacco Resnati - 1950 m/s.l.m. - + 1,9° (integrale + 1,5°)<br />
Sils/Maria - 1798 m/s.l.m. 637,9 (- 30,7 mm ; - 4,6 %) + 0,1° (+ 0,3°)<br />
S.Antonio di Valfurva - 1360 m/s.l.m. 528,2 (+ 42 mm ; + 8,0 %) + 3,5° (+ 0,1°)<br />
Sondrio - 290 m/s.l.m. 589,9 (- 100,1 mm ; - 14,5 %) + 9,1° (- 0,4°)<br />
Andalo Valtellino - 220 m/s.l.m. 752,6 (- 81,5 mm ; - 9,8 %) + 10,1°<br />
Massimeno (TN) - 860 m/s.l.m. 834 (+ 70 mm ; + 10 %) + 6,4°<br />
*Average value for the period October 2007- May 2008 because of an instrument failure in June, 2008