Combined variations of insolation and ice sheet led to major global climatic and ecosystem
changes between the Last Glacial Maximum (LGM) and the Holocene. However, little is …

The dynamics of glacial–interglacial monsoon variability can be attributed to orbitally
induced changes in summer insolation and internal boundary conditions. However, the …

Orbital-scale global climatic changes during the late Quaternary are dominated by high-
latitude influenced~ 100,000-year global ice-age cycles and monsoon influenced~ 23,000 …

Paleoclimatic research can provide critical insight on causes of change in the East Asian
monsoon, which influences the lives of 1.6 billion people today. In this study, we use …

Greenland ice core water isotopic composition (δ18O) provides detailed evidence for abrupt
climate changes but is by itself insufficient for quantitative reconstruction of past …

Understanding the past significant changes of the East Asia Summer Monsoon (EASM) and
Winter Monsoon (EAWM) is critical for improving the projections of future climate over East …

Abstract Projecting how the East Asian summer monsoon (EASM) rainfall will change with
global warming is essential for human sustainability. Reconstructing Holocene climate can …

The sensitivity of the Greenland ice sheet to climate forcing is of key importance in assessing
its contribution to past and future sea level rise. Surface mass loss occurs during summer …

The response of the global water cycle to changes in global surface temperature remains an
outstanding question in future climate projections and in past climate reconstructions. The …

The mid-latitude westerly winds of the Southern Hemisphere play a central role in the global
climate system via Southern Ocean upwelling, carbon exchange with the deep ocean …