Abstract
Following three decades of relative stability, Jakobshavn Isbrae, West Greenland, underwent dramatic thinning, retreat and speed-up starting in 1998. To assess the amount of ice loss, we analyzed 1985 aerial photos and derived a 40 m grid digital elevation model (DEM). We also obtained a 2007 40 m grid SPOT DEM covering the same region. Comparison of the two DEMs over an area of ∼4000km2 revealed a total ice loss of 160 ± 4 km3, with 107 ± 0.2 km3 in grounded regions (0.27 mm eustatic sea-level rise) and 53 ± 4 km3 from the disintegration of the floating tongue. Comparison of the DEMs with 1997 NASA Airborne Topographic Mapper data indicates that this ice loss essentially occurred after 1997, with +0.7 ± 5.6 km3 between 1985 and 1997 and-160 ± 7 km3 between 1997 and 2007. The latter is equivalent to an average specific mass balance of-3.7 ± 0.2 m a-1 over the study area. Previously reported thickening of the main glacier during the early 1990s was accompanied by similar- magnitude thinning outside the areas of fast flow, indicating that the land-based ice continued reacting to longer-term climate forcing.
Cite
CITATION STYLE
Motyka, R. J., Fahnestock, M., & Truffer, M. (2010). Volume change of Jakobshavn Isbrae, West Greenland: 1985-1997-2007. Journal of Glaciology, 56(198), 635–646. https://doi.org/10.3189/002214310793146304
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.