Climatic and glaciological information inferred from air-content measurements of a Law Dome (East Antarctica) ice core
AbstractThe total air content(V)of ice has been measured along the Dome Summit South (DSS) core from Law Dome, East Antarctica. The main features of this record are the very well-preserved sub-annual fluctuations ofV(down to at least 900 m depth) and the significant increase of theVvalues during the last deglaciation. The sub-annual variations reflect changes in close-off porosity, and we interpret theVseasonal peaks as tracers of depth-hoar layers. For the longer time-scale, the largeVfluctuations observed are interpreted in terms of elevation and/or close-off porosity changes under different assumptions. We analyze the possible influence of a different global pressure field and/or a change in seasonal temperature and precipitation cycles during the last glacial period. Our estimates of surface elevation changes derived from theVdata are then compared with independent reconstructions of past elevations.