Spatial and temporal variability in isotope composition of recent snow in the vicinity of Vostok station, Antarctica: implications for ice-core record interpretation

This correlation is mainly determined by slow (50-year) variations, while at short-term time-scale (about 10 years) the isotope composition of snow at Vostok seems to be

A lower Dome C-Vostok ratio (Figure 7) during the glacial period could be interpreted as an accumulation rate decrease greater than expected at Dome C, or lower than expected at

Our strategy is to make an optimal use of the combina- tion of all water stable isotopes (δD, δ 17 O, δ 18 O) in different types of snow on the Antarctic plateau (precipitation,

Natural sea-ice ob- servations suggest that the isolated system assumption holds for a few hours at most, after which rapid heat and salt exchanges mostly destroy the initial

During the two warm summers of 2011 and 2012 at NEEM, continuous measurements of near-surface water vapor com- bined with isotopic measurements of snow samples collected every 12–24

Since the snow cover is in general heterogeneous at any scales from the small scale to the application scale, the actual uncertainty of the snow depth in a given area is much

Dans Liebman, anecdote allemande, nouvelle publiée par Baculard d’Arnaud en 1775, c’est bien encore (mais cette fois de manière totalement implicite), la figure de Rousseau qui,

Many techniques utilized in analyzing and comparing digital filter structures are based on a somewhat more general theory relating to the properties of digital