CHANGE

CHANGE

IN CONVERSATION WITH MICHAEL MATIU

“Projection for the future (2071-2100).
RCP2.6 (left column) is 1.5-2 degrees, RCP8.5 (right column) is 4-5 degrees warmer.
First row (a) are absolute numbers of snow cover duration. Second row (b) are absolute changes in days of snow cover. Third line (c) are relative changes. The blue spots (e.g. Po Valley) theoretically show strong increases > 100%, but we are talking about less than 5 or so days with snow per year.
 In summary, this gives the following picture. For RCP8.5: in absolute terms, annual snow cover is decreasing, especially at high elevations. Relatively speaking, there is hardly any snow at low elevations; there may still be some, but it is extremely unlikely, or only on single years. Relative changes at high altitudes are small, i.e. there will still be snow, but less. In comparison, the changes RCP2.6 are much smaller (third to half as large).” 
Matiu, M., & Hanzer, F. (2022). Bias adjustment and downscaling of snow cover fraction projections from regional climate models using remote sensing for the European Alps. Hydrology and Earth System Sciences, 26(12), 3037–3054. https://doi.org/10.5194/hess-26-3037-2022

 

IMPORTANTE

2021

The tarp presents a statistical graph derived from a scholarly study focused on the snow cover in the Alpine region. The selection of this particular diagram was intentional, aimed at highlighting the significant role and the extensive presence of snow within the Alps. It underscores the critical importance of snow to this geographic area, skillfully avoiding direct reference to the perils brought forth by climate change. Instead, the emphasis is placed on visually representing the profound connection between the Alpine region and its snow coverage. 
 Material: PVC tarpaulin 510g Frontlit tarpaulin, B1 certified – flame retardant according to DIN 4102, 2500 x 1500 mm