Arctic Amplification is a fundamental feature of past, present, and modelled future climate.
However, the causes of this “amplification” within Earth's climate system are not fully …

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 …

Reconstructing past climate seasonality is fundamental to understanding the nature of past
climate changes. This is especially true in the Arctic, where climate is intensely seasonal …

Arctic sea-ice loss is emblematic of an amplified Arctic water cycle and has critical feedback
implications for global climate. Stable isotopes (δ18O, δ2H, d-excess) are valuable tracers …

The Arctic's winter water cycle is rapidly changing, with implications for snow moisture
sources and transport processes. Stable isotope values (δ18O, δ2H, d-excess) of the Arctic …

In situ measurements of water vapour isotopic composition in polar regions has provided
needed constrains of post-deposition processes involved in the archiving of the climatic …

Understanding the relative importance of different water sources that replenish soil water
storage is necessary to assess the vulnerability of sub‐arctic areas to changes in climate …

Deuterium excess and stable oxygen isotopes in precipitation have been widely applied to
trace the source of water vapor. In this study, hydrogen and oxygen isotope analyses of …

The Arctic Ocean is an exceptional environment where hydrosphere, cryosphere, and
atmosphere are closely interconnected. Changes in sea-ice extent and thickness affect …

Snow is a valuable carrier for recording atmospheric information and snowmelt constitutes a
crucial hydrological resource for ecosystem sustainability and human activities. The …