Meteorological conditions over Antarctic blue-ice areas and their influence on the local surface mass balance

This paper addresses the causes of the prevailing meteorological conditions observed over an Antarctic blue-ice area and their effect on the surface m ass balance. Over blue-ice areas, net accumulation is zero and ablation occ urs mainly through sublimation. Sublimation rates are much higher than over adjacent snowfields. The meteorological conditions favourable for high sub limation rates (warm, dry and gusty) are due to the specific orographic set ting of this blue-ice area, with usually a steep upwind mountainous slope c ausing strong adiabatic heating. Diabatic warming due to radiation, and ent rainment of warm air from aloft into the boundary layer augment the warming . The prevailing warm, dry conditions explain roughly 50% of the difference in sublimation, and the different characteristics of blue ice (mainly its lower albedo) the other 50%. Most of the annual sublimation (similar to 70% ) takes place during the short summer (mainly in daytime), with winter abla tion being restricted to occasional warm, dry fohn-like events. The additio nal moisture is effectively removed by entrainment and horizontal advection , which are maximum over the blue-ice area. Low-frequency turbulent motions induced by the upwind mountains enhance the vertical turbulent transports. Strong gusts and high peak wind speeds over blue-ice areas cause high pote ntial snowdrift transports, which can easily remove the total precipitation , thereby maintaining zero accumulation.