The Cryosphere, 8, 1807–1823, 2014 www.the-cryosphere.net/8/1807/2014/ doi:10.5194/tc-8-1807-2014 © Author(s) 2014. CC Attribution 3.0 License. Surface velocity and mass balance of Livingston Island ice cap, Antarctica B. Osmanoglu1,2, F. J. Navarro3, R. Hock1,4, M. Braun5, and M. I. Corcuera3 1Geophysical Institute, University of Alaska Fairbanks, P.O. Box 757320 Fairbanks, Alaska, 99775, USA 2Biospheric Sciences Lab., USRA-NASA GSFC, Mail Stop 618.0, Greenbelt, MD, 20771, USA 3Dept. Matemática Aplicada, ETSI de Telecomunicación, Universidad Politécnica de Madrid, Av. Complutense, 30, 28040 Madrid, Spain 4Department of Earth Sciences, Uppsala University, Geocentrum, Villavägen 16, 75236 Uppsala, Sweden 5Institute of Geography, University of Erlangen, Kochstrasse 4/4, 91054 Erlangen, Germany Correspondence to: B. Osmanoglu (
[email protected]) Received: 30 June 2013 – Published in The Cryosphere Discuss.: 26 August 2013 Revised: 26 July 2014 – Accepted: 8 August 2014 – Published: 8 October 2014 Abstract. The mass budget of the ice caps surrounding of taking into account the seasonality in ice velocities when the Antarctica Peninsula and, in particular, the partition- computing frontal ablation with a flux-gate approach. ing of its main components are poorly known. Here we approximate frontal ablation (i.e. the sum of mass losses by calving and submarine melt) and surface mass balance of the ice cap of Livingston Island, the second largest is- 1 Introduction land in the South Shetland Islands archipelago, and anal- yse variations