A sea ice climate switch mechanism for the 100-kyr glacial cycles

Hezi Gildor*, Eli Tziperman

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

98 Scopus citations

Abstract

A box model of the ocean-atmosphere-sea ice-land ice climate system is used to study a novel mechanism for self-sustained oscillations of the climate system on a time scale of 100,000 years, without external forcing. The oscillation in land ice volume has the familiar sawtooth shape of climate proxy records. The most novel aspect of the climate oscillations analyzed here is the crucial role played by the sea ice. The sea ice acts as a "switch" of the climate system, switching it from a growing land glaciers mode to a retreating land glaciers mode and shaping the oscillation's sawtooth structure. A simple explanation of the 100-kyr timescale is formulated on the basis of the mechanism seen in the model. Finally, rapid sea ice changes such as those seen in our model, and their drastic effects on the climate system, may provide an explanation to some of the rapid climate changes observed to be a part of the variability at all timescales in the paleorecord.

Original languageAmerican English
Article number1999JC000120
Pages (from-to)9117-9133
Number of pages17
JournalJournal of Geophysical Research: Oceans
Volume106
Issue numberC5
DOIs
StatePublished - 15 May 2001
Externally publishedYes

Fingerprint

Dive into the research topics of 'A sea ice climate switch mechanism for the 100-kyr glacial cycles'. Together they form a unique fingerprint.

Cite this