Over the modern satellite era, substantial climatic changes have been observed in the
Antarctic, including atmospheric and oceanic warming, ice sheet thinning and a general …

Earth's tropical and subtropical rainbands, such as Intertropical Convergence Zones (ITCZs)
and monsoons, are complex systems, governed by both large‐scale constraints on the …

This article provides a comprehensive review of the global monsoon that encompasses
findings from studies of both modern monsoons and paleomonsoons. We introduce a …

Here we present a new data synthesis of global peatland ages, area changes, and carbon
(C) pool changes since the Last Glacial Maximum, along with a new peatland map and total …

The present interglacial, the Holocene, spans the period of the last 11,700 years. It has
sustained the growth and development of modern society. The millennial-scale decreasing …

Precise characterization of hydroclimate variability in Amazonia on various timescales is
critical to understanding the link between climate change and biodiversity. Here we present …

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 …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

The Greenland Ice Core Chronology 2005 (GICC05) is a time scale based on annual layer
counting of high-resolution records from Greenland ice cores. Whereas the Holocene part of …

The regional monsoons of the world have long been viewed as seasonal atmospheric
circulation reversal—analogous to a thermally-driven land-sea breeze on a continental …