This paper provides an updated review of the most relevant scientific literature related to the
hydroclimate of the Andes. The Andes, the longest cordillera in the world, faces major …

The new excess term of the triple oxygen isotope composition in meteoric water, expressed
as∆′ 17 O, is conceived to track the component of kinetic fractionation in the water cycle …

The water cycle over the Amazon basin is a regulatory mechanism for regional and global
climate. The atmospheric moisture evaporated from this basin represents an important …

Previous studies have estimated that 25%–35% of Amazonian precipitation comes from
evapotranspiration (ET) within the basin. However, due to simplifying assumptions of …

The deuterium excess (d‐excess) of precipitation varies seasonally at sites across the globe,
an observation that has often been linked to seasonal changes in oceanic evaporation …

Monitoring studies are necessary to better understand the hydrological processes affecting
the isotopic signature of cave waters, which are ultimately recorded in speleothems that are …

Changes in Normalized Difference Vegetation Index in the Orinoco and Amazon River Basins:
Links to Tropical Atlantic Surface Temperatures in: Journal of Climate Volume 33 Issue 19 …

Speleothem oxygen isotope (δ 18 O) records provide key insight into the rate and timing of
terrestrial paleoclimate changes during the late Quaternary. However, it can be difficult to …

Defining moisture sources and evolution of precipitation is of significance for further
exploration of complex hydro‐climatic interactions, especially under global warming with …

Extant climate observations suggest the dry season over large parts of the Amazon Basin
has become longer and drier over recent decades. However, such possible intensification of …