In January 1980, the accumulation rates on the Filchner/Ronne ice shelves and at Atka Bay were determined by snow-pit stratigraphy (at Filchner station) and isotope analyses using a snow pit and a handdrilled core down to about 12 m from the surface. At Filchner station a mean annual net accumulation of 51 cm a −1 of snow representing a water equivalent of 20 g cm −2 was found by stratigraphic measurements. 2 H, 18 0 and 3 H analyses led to a value of 55 cm a −1 of snow for the last two decades. At Atka Bay a mean annual accumulation rate of 75 cm a −1 of snow resulted from 2 H and 18 0 analyses.
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Reinwarth et al. (1982) studied this question.
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