Asian summer monsoon (ASM) variability significantly affects hydro-climate, and thus socio-
economics, in the East Asian region, where nearly one-third of the global population resides …

Climate changes across the past 24,000 years provide key insights into Earth system
responses to external forcing. Climate model simulations, and proxy data,,,,–have …

Abstract The Last Glacial Maximum (LGM), one of the best studied palaeoclimatic intervals,
offers an excellent opportunity to investigate how the climate system responds to changes in …

The climatic controls on the stable carbon isotopic composition (δ 13 C) of speleothem
carbonate are less often discussed in the scientific literature in contrast to the frequently …

Stalagmites are an extraordinarily powerful resource for the reconstruction of climatological
palaeoseasonality. Here, we provide a review of different types of seasonality preserved by …

Characterizing the temporal uncertainty in palaeoclimate records is crucial for analysing
past climate change, correlating climate events between records, assessing climate …

Speleothem oxygen isotopic (δ18O) records are used to reconstruct past hydroclimate yet
records from the same cave do not always replicate. We use a global database of …

Palaeoclimate information on multiple climate variables at different spatiotemporal scales is
becoming increasingly important to understand environmental and societal responses to …

We present here the first results, for the preindustrial and mid-Holocene climatological
periods, of the newly developed isotope-enhanced version of the fully coupled Earth system …

In recent decades speleothems have become valuable climate archives and are of crucial
importance for the investigation of past climate conditions. Albeit much progress has been …