Astronomy and Astrophysics – Astronomy
Scientific paper
Sep 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002natur.419..199l&link_type=abstract
Nature, Volume 419, Issue 6903, pp. 199-206 (2002).
Astronomy and Astrophysics
Astronomy
52
Scientific paper
The oscillations between glacial and interglacial climate conditions over the past three million years have been characterized by a transfer of immense amounts of water between two of its largest reservoirs on Earth - the ice sheets and the oceans. Since the latest of these oscillations, the Last Glacial Maximum (between about 30,000 and 19,000 years ago), ~50 million cubic kilometres of ice has melted from the land-based ice sheets, raising global sea level by ~130 metres. Such rapid changes in sea level are part of a complex pattern of interactions between the atmosphere, oceans, ice sheets and solid earth, all of which have different response timescales. The trigger for the sea-level fluctuations most probably lies with changes in insolation, caused by astronomical forcing, but internal feedback cycles complicate the simple model of causes and effects.
Esat Tezer M.
Lambeck Kurt
Potter Emma-Kate
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