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Spectral analysis has been applied to study the time- and space-series of snow accumulation obtained by stake measurements at Vostok station (Antarctica). The intermediate-scale surface undulations drifting across the stake field are found to be primary responsible for the oscillations of snow accumulation recorded at a single point. Application of the results to the stratigraphie studies is discussed.
Translated title of the contribution | Temporal and spatiat aum-tui-e of snow accumulation field at the vicinity of Vostok station, Central Antarctida |
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Original language | Russian |
Pages (from-to) | 38-XIII |
Journal | Vestnik - Sankt-Petersburgskogo Universiteta, Seriya Geologiya i Geografiya |
Volume | 7 |
Issue number | 4 |
State | Published - 1 Dec 1998 |
ID: 61461786