The hydrologic cycle is a fundamental component of the climate system with critical societal
and ecological relevance. Yet gaps persist in our understanding of water fluxes and their …

Water-stable isotopes in polar ice cores are a widely used temperature proxy in
paleoclimate reconstruction, yet calibration remains challenging in East Antarctica. Here, we …

The glacial-interglacial variability of precipitation and its driving mechanism in monsoonal
regions has long been a subject of debate. However, there are few records of quantitative …

Global climate change varies greatly in different regions, so it is necessary to
comprehensively analyze climate change in different regions through different indicators …

A continuous high-resolution record from a precisely-dated stalagmite spanning the last
precessional cycle provides new insight into the dynamics of climate change from orbital to …

One long-standing issue in the paleoclimate records is whether East Asian Summer
Monsoon peaked in the early Holocene or mid-Holocene. Here, combining a set of transient …

Abstract How fast the Northern Hemisphere (NH) forest biome tracks strongly warming
climates is largely unknown. Regional studies reveal lags between decades and millennia …

The Caucasus region is key for understanding early human dispersal and evolution in
Eurasia, and characterizing the environmental contrast between Last Glacial Maximum and …

As the most dominant tropical climate mode on the interannual time scale, El Niño–Southern
Oscillation (ENSO) is suggested to significantly influence the interannual variation of East …

Speleothem oxygen isotope (δ18Oc) records have been regarded as a critical reference to
study past Asian monsoon variability. However, existing δ18Oc records in the Indian …