As part of a long-term mass-balance program run by SWEDARP since 1988, a detailed study on Plogbreen, Dronning Maud Land, Antarctica, was undertaken during the austral summer of 2003 to investigate the long-term mass balance. We compare ice outflux, φ_out, through a cross-sectional gate with ice influx, φ_in, from the upstream catchment area. The φ_in is based on calculations of snow accumulation upstream of the gate using data available from published ice-core records. The φ_out is based on Glen's flow law aided by thermodynamic modeling and force-budget calculations. Input data from the field consist of measurements of ice surface velocity and ice geometry. The ice surface velocity was measured using repeated differential global positioning system surveying of 40 stakes over a period of 25 days. The ice geometry was determined by 174 km of ground-penetrating radar profiling using ground-based 8 MHz dipole antennas. This study presents the collected velocity and geometry data as well as the calculated ice flux of Plogbreen. The results show a negatively balanced system within the uncertainty limits; φ_out = 0.55 ± 0.05 km³ a⁻¹ and φ_in = 0.4 ± 0.1 km³ a⁻¹. We speculate that the negative balance can be explained by recent eustatic increase reducing resistive stresses and inducing accelerated flow.