We investigate the spectral properties of climatic times series derive
d from two recent ice cores in Greenland and East Antarctica. We find
that the signals behave in a similar way in the high frequency part of
their spectra. The rapid oscillations found in the GRIP ice core were
closely correlated to Heinrich Events. A comparable spectra feature i
s detected in the Vostok ice core. We discuss the possibilities of con
nections between the two hemispheres and proper ice sheet oscillations
in the light of simple oscillating climate models.