Abstract Late Pleistocene and Holocene ground ice are common throughout the Arctic.
Some forms of relict ground ice preserve local meteoric water, and their stable oxygen‐and …

Over the past few decades, the δ 18 O records of ice wedges have been used to estimate
late Quaternary winter air temperatures. This study first reviews the development of ice …

Climatic warming has resulted in permafrost degradation and it is expected to alter the
hydrological processes and hydraulic connectivity on the Qinghai-Tibet Plateau (QTP) …

Climate change and thawing permafrost in the Arctic will significantly alter landscape hydro‐
geomorphology and the distribution of soil moisture, which will have cascading effects on …

Eastern Beringia is one of the few Western Arctic regions where full Holocene climate
reconstructions are possible. However, most full Holocene reconstructions in Eastern …

Abstract Morphologic features, 600–1100 m across and elevated up to 30 m above the
surrounding seafloor, interpreted to be mud volcanoes were investigated on the continental …

Water is the most important factor limiting the growth of sand-binding vegetation (SBV) in
desert ecosystems. This study explored the water sources and water use strategies of SBV …

Herschel Island in the southern Beaufort Sea is a push moraine at the northwestern‐most
limit of the Laurentide Ice Sheet. Stable water isotope (δ18O, δD) and hydrochemical studies …

The composition of perennially frozen deposits holds information on the palaeo-environment
during and following deposition. In this study, we investigate late Pleistocene permafrost at …

Stable isotopic tracing has proven to be a useful tool for assessing surface water source
dynamics and hydrological connectivity in permafrost regions. This study has investigated …