To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …

The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …

We present a new time‐slice reconstruction of the Eurasian ice sheets (British–Irish,
Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …

This is the first part of a two-paper series presenting the Global Streamflow Indices and
Metadata archive (GSIM), a worldwide collection of metadata and indices derived from more …

Ice-marginal moraines are often used to reconstruct the dimensions of former ice masses,
which are then used as proxies for palaeoclimate. This approach relies on the assumption …

GIS-based reconstructions of Lake Onego development in the Late Pleistocene and the
Holocene are presented. Reconstructions originated from the ideas of the Lake Onego …

The timing of past glaciation across the Tian Shan provides a proxy for past climate change
in this critical area. Correlating glacial stages across the region is difficult but cosmogenic …

Aeolian sediments and landforms of the former continental ice sheets' periphery can be
used as invaluable sources of information on palaeoenvironmental changes. In the …

We describe and discuss the glacial and climate variations in the Polar Ural Mountains in
northern Russia over the last 100 000 years. A series of optically stimulated luminescence …

ABSTRACT The Severnaya Dvina River valley crosses the former south‐eastern margin of
the last Scandinavian Ice Sheet. Despite a long research history, there remains …