Over the past 50 years, retreating glaciers and ice caps contributed 0.5 mm yr-1to sea-level rise, and one third of this contribution is believed to come from ice masses bordering the Gulf of Alaska. However, these estimates of ice loss in Alaska are based on measurements of a limited number of glaciers that are extrapolated to constrain ice wastage in the many thousands of others. Uncertainties in these estimates arise, for example, from the complex pattern of decadal elevation changes at the scale of individual glaciers and mountain ranges. Here we combine a comprehensive glacier inventory with elevation changes derived from sequential digital elevation models. We find that between 1962 and 2006, Alaskan glaciers lost 41.9 ± 8.6 km 3yr-1 of water, and contributed 0.12 ± 0.02 mm yr-1 to a-level rise, 34% less than estimated earlier2,3. Reasons for our lower values include the higher spatial resolution of our glacier inventory as well as the reduction of ice thinning underneath debris and at the glacier margins, which were not resolved in earlier work. We suggest that estimates of mass loss from glaciers and ice caps in other mountain regions could be subject to similar revisions.
|Original language||English (US)|
|Number of pages||4|
|State||Published - Feb 2010|
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)