In an attempt to find potential interglacial analogues of our present interglacial and its
natural future, five interglacials (MIS-1, 5, 9, 11 and 19) are studied in terms of their …

The “paleo calendar effect” is a common expression for the impact that changes in the length
of months or seasons over time, related to changes in the eccentricity of Earth's orbit and …

The timing of ice ages over the past∼ 2,600 thousand years (kyr) follows pacing by cyclical
changes in three aspects of Earth's orbit that influence the solar energy received as a …

Earth climate is changing! For geoscientists who probe the sedimentary and ice
paleoclimate archives, this will be old news. Since the onset of major glaciations in the …

The last 6000years are of particular interest to the understanding of the Earth System
because the boundary conditions of the climate system did not change dramatically (in …

Abstract Late Paleozoic glaciation on Gondwana is associated with changes in geography,
solar luminosity, and estimated CO2 levels. To assess the relative importance of these …

Deciphering the evolution of global climate from the end of the Last Glacial Maximum
approximately 19 ka to the early Holocene 11 ka presents an outstanding opportunity for …

A Community Climate System Model, Version 3 (CCSM3) simulation for 125 ka during the
Last Interglacial (LIG) is compared to two recent proxy reconstructions to evaluate surface …

It is commonly accepted that the variations of Earth's orbit and obliquity control the timing of
Pleistocene glacial–interglacial cycles. Evidence comes from power spectrum analysis of …

The recent development of continuous paleoclimatic reconstructions covering hundreds of
thousands of years paved the way for a large number of studies from disciplines ranging …