Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

Atmospheric water vapour residence time (WVRT) is an essential indicator of how
atmospheric dynamics and thermodynamics mediate hydrological cycle responses to …

Anthropogenic climate change is currently driving environmental transformation on a scale
and at a pace that exceeds historical records. This represents an undeniably serious …

The loss of Arctic sea-ice has been implicated with severe cold and snowy mid-latitude
winters. However, the mechanisms and a direct link remain elusive due to limited …

Deuterium excess (d-excess) is a second-order stable isotope parameter measured in
meteoric water to understand both the source of precipitation and the evolution of moisture …

Studying the evaporation process and its link to the atmospheric circulation is central for a
better understanding of the feedbacks between the surface water components and the …

Aemisegger, F., Sturm P., Graf P., Sodemann H., Pfahl S., Knohl A., and Wernli H., 2012:
Measuring variations of δ 18 O and δ 2 H in atmospheric water vapour using two commercial …

This paper presents a continental scale interpretation of δ 2 H and δ 18 O in Australian
precipitation, incorporating historical GNIP data at seven sites (1962–2002) and 8–12 years …

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 …

Water resources in the northwestern Himalayas are influenced by the circulation of two
dominant weather systems: westerlies and southwest monsoons. The effect of climate …