The Antarctic ice sheet is Earth's largest reservoir of fresh water. Accurate estimates of its mass variability, accompanied by realistic error bars, would greatly reduce current uncertainties in projected sea-level change, with obvious societal and economic impacts. There have been substantial improvements in monitoring the ice sheet in the past few years (1–3), although recent studies have provided contrasting mass balance estimates (1, 3).
Antarctic mass variability is difficult to measure because of the ice sheet's size and complexity. Previous estimates have used a variety of techniques (1), each with intrinsic limitations and uncertainties. A problem common to all these techniques is the difficulty of monitoring the entire ice sheet. Studies that rely on a single method can provide estimates for only a portion of the ice sheet, and even studies that synthesize results from several techniques suffer from sparse data in critical regions.
The most recent Intergovernmental Panel on Climate Change (IPCC) assessment estimated that the Antarctic contribution to sea-level rise during the past century was 0.2 ± 0.3 mm/year (2). The report predicted that the Antarctic ice sheet will probably gain mass during the 21st century because of increased precipitation in a warming global climate. Recent radar altimeter measurements (3) have shown an increase in the overall thickness of the East Antarctic Ice Sheet's (EAIS's) interior during 1992–2003. However, the IPCC prediction does not consider possible dynamic changes in coastal regions, and radar altimetry provides only sparse coverage of those areas (2). Detailed interferometric synthetic-aperture radar and airborne laser altimeter surveys of glaciers along the edge of the West Antarctic Ice Sheet (WAIS) show rapid increases in near-coastal discharge during the past few years (4). The overall contribution of the Antarctic ice sheet to global sea-level change thus depends on the balance between mass changes in the interior and those in coastal areas (1). The gravitational survey of Antarctica provided by the Gravity Recovery and Climate Experiment (GRACE) satellites and discussed in this paper is a comprehensive survey of the entire ice sheet and is thus able to overcome the issue of limited sampling.