ABSTRACT. We calculate the present ice budget for Antarctica from measurements of accumulation minus iceberg calving, run-ofT and in situ meltin~ beneath the floating ice shelves . The resulting negative mass balance of 469 Gt yeardifTers substantially from other recent estimates but some components are subject to high temporal variability and budget uncertainties of20-50%. Annual accumulation from an earlier review is adjusted to include the Antarctic Peninsula for a total of 2144Gtyear-l . An iceberg production rate of 2016 Gtyear-I is obtained from the volume of large icebergs calculated from satellite images since 1978, and from the results of an international iceberg census project. Ice-shelf melting of 544 Gt year-I is derived from physical and geochemical observations of meltwater outflow, glaciological field studies and modeling of the sub-ice ocean circulation. The highest melt rates occur near ice fronts and deep within sub-ice cavities. Run-ofT from the ice-sheet surface and from beneath the grounded ice is taken to be 53 Gt year-I. Less than half of the negative mass balance need come from the grounded ice to account for the unattributed 0.45 mm year-I in the IPCC "best estimate" of the recent global sea-level rise.

We calculate the present ice budget for Antarctica from measurements of accumulation minus iceberg calving, run-off and in situ melting beneath the floating ice shelves. The resulting negative mass balance of 469 Gt year−1differs substantially from other recent estimates but some components are subject to high temporal variability and budget uncertainties of 20–50%. Annual accumulation from an earlier review is adjusted to include the Antarctic Peninsula for a total of 2144 Gt year−1. An iceberg production rate of 2016 Gt year−1is obtained from the volume of large icebergs calculated from satellite images since 1978, and from the results of an international iceberg census project. Ice-shelf melting of 544 Gt year−1is derived from physical and geochemical observations of meltwater outflow, glaciological field studies and modeling of the sub-ice ocean circulation. The highest melt rates occur near ice fronts and deep within sub-ice cavities. Run-off from the ice-sheet surface and from beneath the grounded ice is taken to be 53 Gt year−1. Less than half of the negative mass balance need come from the grounded ice to account for the unattributed 0.45 mm year−1in the IPCC “best estimate” of the recent global sea-level rise.