Articles | Volume 8, issue 6
https://doi.org/10.5194/tc-8-2235-2014
https://doi.org/10.5194/tc-8-2235-2014
Research article
 | 
02 Dec 2014
Research article |  | 02 Dec 2014

Post-LIA glacier changes along a latitudinal transect in the Central Italian Alps

R. Scotti, F. Brardinoni, and G. B. Crosta

Viewed

Total article views: 4,077 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,992 1,881 204 4,077 159 156
  • HTML: 1,992
  • PDF: 1,881
  • XML: 204
  • Total: 4,077
  • BibTeX: 159
  • EndNote: 156
Views and downloads (calculated since 22 Jul 2014)
Cumulative views and downloads (calculated since 22 Jul 2014)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 21 Nov 2024
Download
Short summary
A post-LIA multitemporal glacier inventory along a latitudinal transect in the Central Italian Alps shows that average annual decrease (AAD) in glacier area has risen by about ten times from 1860--1990 to 1990--2007. When considering glaciers smaller than 0.5 km2, post-1990 AAD follows the latitudinal gradient with maritime-like Orobie glaciers shrinking much less than Disgrazia and Livigno glaciers. We argue that the recent resilience of glaciers in Orobie is due to local climatic decoupling.