Understanding Holocene climate variability is crucial for predicting future climate change,
which will disproportionally affect high-latitude regions. Summer temperature (T summer) …

Terrestrial temperature exerts a major influence on vegetation distribution, the hydrologic
cycle and many biogeochemical cycles. Yet little research into terrestrial paleo-temperature …

A mismatch between model-and proxy-based Holocene climate change, known as the
“Holocene conundrum”, may partially originate from the poor spatial coverage of climate …

Here we describe LegacyClimate 1.0, a dataset of the reconstruction of the mean July
temperature (T July), mean annual temperature (T ann), and annual precipitation (P ann) …

Numerical simulations employing prognostic stable water isotopes can not only facilitate our
understanding of hydrological processes and climate change but also allow for a direct …

The Greenland Ice Sheet is a large contributor to global sea-level rise, and current mass
losses are projected to accelerate. However, model projections of future ice-sheet evolution …

Abstract The East Asian summer monsoon (EASM) is a key component of the global
monsoon system, with significant impacts on the climate and ecosystems in Taiwan …

Abstract The influence of Holocene East Asian Summer Monsoon (EASM) rainfall on
ecosystems over northern China remains controversial: delay or synchronization. Here we …

Understanding Holocene temperature changes is vital for resolving discrepancies between
proxy reconstructions and climate models. The intricate temperature variations across the …

Here we describe the LegacyClimate 1.0, a dataset of the reconstruction of mean July
temperature (T July), mean annual temperature (T ann), and annual precipitation (P ann) …