C21B-0315:
Recent Changes in Ices Mass Balance of the Amundsen Sea Sector
Tuesday, 16 December 2014
Tyler C Sutterley1, Isabella Velicogna2, Eric J Rignot1, Jeremie Mouginot1, Thomas Flament3, Michiel R van den Broeke4, Melchior van Wessem5 and Carleen Reijmer6, (1)University of California Irvine, Irvine, CA, United States, (2)University of California Irvine, Department of Earth System Science, Irvine, CA, United States, (3)University of Leeds, School of Earth and Environment, Leeds, United Kingdom, (4)Utrecht University, Utrecht, Netherlands, (5)Institute for Marine and Atmospheric Research Utrecht, Utrecht, 3584, Netherlands, (6)Institute for Marine and Atmospheric Research Utrecht, Utrecht, Netherlands
Abstract:
The glaciers flowing into the Amundsen Sea Embayment (ASE) sector of West Antarctica were confirmed in the Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE) to be the dominant contributors to the current Antarctic ice mass loss, and recently recognized to be undergoing marine ice sheet instability. Here, we investigate their regional ice mass balance using a time series of satellite and airborne data combined with model output products from the Regional Atmospheric and Climate Model (RACMO). Our dataset includes laser altimetry from NASA’s ICESat-1 satellite mission and from Operation IceBridge (OIB) airborne surveys, satellite radar altimetry data from ESA’s Envisat mission, time-variable gravity data from NASA/DLR’s GRACE mission, surface mass balance products from RACMO, ice velocity from a combination of international synthetic aperture radar satellites and ice thickness data from OIB. We find a record of ice mass balance for the ASE where all the analyzed techniques agree remarkably in magnitude and temporal variability. The mass loss of the region has been increasing continuously since 1992, with no indication of a slow down. The mass loss during the common period averaged 91 Gt/yr and accelerated 20 Gt/yr2. In 1992-2013, the ASE contributed 4.5 mm global sea level rise. Overall, our results demonstrate the synergy of multiple analysis techniques for examining Antarctic Ice Sheet mass balance at the regional scale. This work was performed at UCI and JPL under a contract with NASA.
