Dienstag, 26. August 2008
Mittwoch, 13. August 2008
PermaNET
Bolzano/Bozen, Italy
The conference will give an overview of the effects of climate change to permafrost in the Alps. The PermaNET (Permafrost Long-Term Monitoring Network) project will be presented.
The event will be the start meeting of the PermaNET project. The public session in the morning will give an overview of the observed effects of climate changes to permafrost in different parts of the Alps (Italy, France, Austria and Swiss). Practical approaches for dealing with the related slope instabilities and natural hazards will be presented and the needs for monitoring activities will be highlighted. In the closing session, an outlook on the planned activities within the PermaNET project and on the expected results will be given.
Samstag, 12. Juli 2008
Sin flood
The Wildspitz, highest mountain in the Ötztaler Alps with 3772m, and the tongue of the Hintereis-glacier descending in the valley of RofenThe mountain group of the Ötztaler Alps are one of the most studied sites in climatology and glaciers-history. Historic mention and description about local glaciers are known at least for the last 300 years.
This glacier is famous for its repeated catastrophic advances, interpreted as surge-events. These surging advances damned the meltwater of nearby glaciers in the main valley, resulting in catastrophic floods which have been documented since 1600 A.D. and which caused heavy damage and loss of property, particularly in the years 1600, 1678, 1680, 1773, 1845, 1847 and 1848. The lake was called after the valley that branches from the Vernagt-valley “Lake Rofen (after the Rofen-valley)”.
Reconstructing of the glacier extent in the postglacial until the last highstand of 1850 (red lines). Note the tongue of the Vernagtferner protruding in the valley of Rofen (ca. 10°50`E and 46°50`N).KRAINER & SPIELER (1999): The sedimentary record of ice-damned lakes in the Ötztal Alps (Austria). Zeitschrift für Gletscherkunde und Glazialgeologie. Bd.35(1)
Sonntag, 22. Juni 2008
Cold-Climate Landforms on Mars

Samstag, 21. Juni 2008
Beware of the Blob!
Indescribable....
.....Indestructible
........Nothing can stop it!
But, like always, every monster, after killing some people, encounter his hero, and fail at his weak point. In this case, low temperatures!Freitag, 13. Juni 2008
Glaciers from outer space !!!

It is a world covered entirely in snow and ice, with numerous moons, and pelted by meteorites from a nearby asteroid belt. But even on this frozen planet, you still can find an entire ecosystem, the tauntaun, a 2,5m tall bipedal herbivore, grazing on lichens, and hunted by the terrible Wampa. Wampas are mainly solitary hunters, like the polar bear (Ursus maritimus) from the planet earth, an example of convergent evolution.
Similarities of the scenery in the movie with the moon Europa are also unintentional.
Dienstag, 10. Juni 2008
Climate Change in Art
There are a lot of pictures rappresenting different landscapes with views of glaciers - and surely I will dedicate them an apposite post in future times - showing how men was inspired by them, or what men think(ed) about glaciers (other imagines show what glaciers think about our behaviour on them...)
A ice related picture is the "The Sea of Ice" or "Polar Sea" (mistakenly confused with "The Wreck of Hope", "The Wreck of the North Pole Expedition"), painted 1823-25.
The picture appears by itself cold and lost, seems frozen for all eternity in time. It was maybe inspired of the pronounced shift to a more humid and cold climate seen between 1500 and 1850 (the so called Little Ice Age), with glacier advances and for long periods frozen (North)sea and rivers.
A known masterpiece of Bruegel shows a Winter Landscape with a Bird Trap (painted 1565). This picture is climate related for the fact, that it´s shows a frozen river, with people enjoying skating on it. Today only in the most severe winter this could be possible in the Netherlands. But between 1500 to 1600 it happened regularly, so that the rivers where used in the winter like streets.
