Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

Glacial–interglacial cycles are global climatic changes which have characterized the last 3
million years. The eight latest glacial–interglacial cycles represent changes in sea level over …

Climate over the past million years has been dominated by glaciation cycles with periods
near 23,000, 41,000, and 100,000 years. In a linear version of the Milankovitch theory, the …

Marked by a progressive increase in the amplitude of climate oscillations, an evolving
waveform, and a shift towards a quasi-100 ky frequency, the Early–Middle Pleistocene …

The increase in atmospheric CO2 levels during the last deglaciation was comparable in
magnitude to the recent historical increase. However, global CO2 budgets for these changes …

This book introduces stochastic dynamical systems theory in order to synthesize our current
knowledge of climate variability. Nonlinear processes, such as advection, radiation and …

The evolution of interocean carbon isotopic gradients over the last 2.5 my is examined using
high-resolution δ 13 C records from deep sea cores in the Atlantic and Pacific Oceans. Over …

The origin of the 100 kyr cyclicity, which dominates ice volume variations and other climate
records over the past million years, remains debatable. Here, using a comprehensive Earth …

The mid-Pleistocene revolution (MPR) is the term used to describe the transition between 41
ka and 100 ka glacial-interglacial cycles which occurred about one million years ago …

Abstract Variations in the eccentricity (100,000 yr), obliquity (41,000 yr) and precession
(23,000 yr) of Earth's orbit have been linked to glacial–interglacial climate cycles. It is …