We developed a multi-mission satellite altimetry analysis over the Antarctic Ice Sheet which
comprises Seasat, Geosat, ERS-1, ERS-2, Envisat, ICESat and CryoSat-2. After a consistent …

The largest uncertainty in future projections of sea level change comes from the uncertain
response of the Antarctic Ice Sheet to the warming oceans and atmosphere. The ice sheet …

We present spatiotemporal mass balance trends for the Antarctic Ice Sheet from a statistical
inversion of satellite altimetry, gravimetry, and elastic‐corrected GPS data for the period …

Abstract Fluctuations in Antarctic Ice Sheet elevation and mass occur over a variety of time
scales, owing to changes in snowfall and ice flow. Here we disentangle these signals by …

Estimating the relative contributions of the atmospheric and dynamic components of ice‐
sheet mass balance is critical for improving projections of future sea level rise. Existing …

We use data acquired between 1978 and 2008 by four satellite radar altimeter missions
(Seasat, ERS‐1, ERS‐2 and Envisat) to determine multidecadal elevation change rates …

This study focuses on the present-day surface elevation of the Greenland and Antarctic ice
sheets. Based on 3 years of CryoSat-2 data acquisition we derived new elevation models …

We use 3 years of Cryosat‐2 radar altimeter data to develop the first comprehensive
assessment of Antarctic ice sheet elevation change. This new data set provides near …

From approximately 400 glaciers of the western Antarctic Peninsula, no in situ records of
mass balance exist and their recent contribution to sea level is consequently poorly …

We analyzed Antarctic ice-sheet elevation change (dH/dt) from 1995 to 2000 using 123
million elevation change measurements from European Remote Sensing 2 ice-mode …