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Objective Climate fluctuations over suborbital or millennial timescale display significant instability during the last glacial period,which are often superimposed upon the orbital periodicity.They triggered some abrupt climate events,such as the Dansgarrd/Oeschger(D-O)events recorded in the Greenland ice cores and the Heinrich(H)
Objective Climate fluctuations over suborbital or millennial timescale display significant instability during the last glacial period, which are often superimposed upon the orbital periodicity. They triggered some abrupt climate events, such as the Dansgarrd / Oeschger (DO) events recorded in the Greenland ice cores and the Heinrich (H)