The limited availability of high-resolution continuous archives, insufficient chronological
control, and complex hydro-climatic forcing mechanisms lead to many uncertainties in …

Several stalagmite records have yielded important but discontinuous insights into northern
Iberian climate since the Last Glacial. Here we present the first continuous Iberian stalagmite …

The Muslim expansion in the Mediterranean basin was one the most relevant and rapid
cultural changes in human history. This expansion reached the Iberian Peninsula with the …

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 …

Stable isotopes of hydrogen and oxygen (δ 2 H, δ 18 O and δ 17 O) can be used as natural
tracers to improve our understanding of hydrological and meteorological processes. Studies …

Abstract Characterization of moisture origins is crucial to understanding hydroclimatic
processes. Nevertheless, documenting past atmospheric moisture contents and their …

The oxygen isotope composition of speleothems is a widely used proxy for past climate
change. Robust use of this proxy depends on understanding the relationship between …

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

Deuterium (δD) and oxygen (δ 18 O) isotopes are powerful tracers of the hydrological cycle
and have been extensively used for paleoclimate reconstructions as they can provide …

Excess surface water on roadways due to storm events can cause hazardous scenarios for
traffic. The design of efficient road and transportation facility drainage systems is a major …