PUBLICATIONS
Location of the 63 surveyed glaciers, labeled in white, overlaid on the topography of (A) NPIand (B) SPI, derived from SRTM of February 2000. Drainage boundaries between glaciers are indicated in red. Elevation  contours in gray lines are separated by 100
Contribution of the Patagonia Icefields of South America to Sea Level Rise
Eric Rignot1,2, Andrés Rivera1,3 and Gino Casassa1
1Centro de Estudios Científicos
2NASA Jet Propulsion Laboratory's Radar
Science and Engineering Section
3Departamento de Geografía, Universidad de Chile
Science, 302, 434-437 (2003).

Digital elevation models of the Northern and Southern Patagonia Icefields of South America generated from  the 2000 Shuttle Radar Topography Mission were compared with earlier cartography to estimate the volume change of the largest 63 glaciers. During the period 1968/1975-2000, these glaciers lost ice at a rate equivalent to a sea level rise of 0.042 ± 0.002 millimeters per year. In the more recent years 1995-2000,  average ice thinning rates have more than doubled to an equivalent sea level rise of 0.105 ± 0.011 millimeters per year. The glaciers are thinning more quickly than can be explained by warmer air temperatures and decreased precipitation, and their contribution to sea level per unit area is larger than that of Alaska glaciers.