Recent contributions of glaciers and ice caps to sea level rise, from GRACE

• Main Authors: Jacob, Thomas, Wahr, J., Pfeffer, T., Swenson, S.
• Other Authors: Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder -National Oceanic and Atmospheric Administration (NOAA), Institute of Arctic and Alpine Research (INSTAAR), University of Colorado Boulder, National Center for Atmospheric Research Boulder (NCAR)
• Format: Other/Unknown Material
• Language: English
• Published: HAL CCSD 2011
• Subjects: geo; envir; Antarctic; Greenland; Antarc*
• Online Access: https://hal-brgm.archives-ouvertes.fr/hal-00633384/file/abstract.pdf; https://hal-brgm.archives-ouvertes.fr/hal-00633384

Glaciers and ice caps (GIC) are important contributors to present-day global mean sea-level rise (SLR). Most previous global mass balance estimates for GIC rely on interpolation of sparse mass balance measurements, representing a small fraction of the GIC area. Instead, we here perform a global, simultaneous inversion of mass change over all ice-covered regions larger than 100 km2 using monthly GRACE-derived satellite gravity fields spanning January 2003 to December 2010. This is the first GRACE-based study where every such GIC region is considered and the results quantified. We conclude that GIC, excluding the Greenland and Antarctic peripheral glaciers and ice caps (PGIC), lost mass at a rate of 148 ± 30 giga tonnes per year (Gt/yr) during this period, contributing 0.41 ± 0.08 mm/yr to SLR. This rate is significantly smaller than previous estimates that rely on extrapolation of mass balance measurements.