Regional glacial-isostatic adjustment in Antarctica inferred from combining space borne geodetic observations (ESA-STSE CryoSat + Project REGINA)

A major uncertainty in determining the mass balance of the Antarctic ice sheet from satellite gravimetry, and to a lesser extent altimetry, measurements is the poorly known correction for the glacial isostatic adjustment (GIA) of the solid Earth. Although much progress has been made in consistently...

Full description

Bibliographic Details
Main Authors: Sasgen, I., Martin, A., Horvath, A., Klemann, V., Petrie, E., Wouters, B., Horwath, M., Pail, R., Bamber, J., Clarke, P., Konrad, H., Drinwater, M.
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_1503947