资源环境科技发展态势分析平台

Changes in accumulated snowfall over the Antarctic Ice Sheet have an immediate and time-delayed impact on global mean sea level. The immediate impact is due to the instantaneous change in freshwater storage over the ice sheet, whereas the time-delayed impact acts in opposition through enhanced ice-dynamic flux into the ocean(1). Here, we reconstruct 200 years of Antarctic-wide snow accumulation by synthesizing a newly compiled database of ice core records(2) using reanalysisderived spatial coherence patterns. The results reveal that increased snow accumulation mitigated twentieth-century sea-level rise by similar to 10 mm since 1901, with rates increasing from 1.1 mm decade(-1) between 1901 and 2000 to 2.5 mm decade(-1) after 1979. Reconstructed accumulation trends are highly variable in both sign and magnitude at the regional scale, and linked to the trend towards a positive Southern Annular Mode since 1957(3). Because the observed Southern Annular Mode trend is accompanied by a decrease in Antarctic Ice Sheet accumulation, changes in the strength and location of the circumpolar westerlies cannot explain the reconstructed increase, which may instead be related to stratospheric ozone depletion(4). However, our results indicate that a warming atmosphere cannot be excluded as a dominant force in the underlying increase.