[HTML][HTML] Deglaciation of fennoscandia
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 …
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …
[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
The last Eurasian ice sheets–a chronological database and time‐slice reconstruction, DATED‐1
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 …
Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …
[HTML][HTML] The build-up, configuration, and dynamical sensitivity of the Eurasian ice-sheet complex to Late Weichselian climatic and oceanic forcing
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 …
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Geophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciation
H Patton, K Andreassen, LR Bjarnadóttir… - Reviews of …, 2015 - Wiley Online Library
Our understanding of processes relating to the retreat of marine‐based ice sheets, such as
the West Antarctic Ice Sheet and tidewater‐terminating glaciers in Greenland today, is still …
the West Antarctic Ice Sheet and tidewater‐terminating glaciers in Greenland today, is still …
A postglacial relative sea-level database for the Russian Arctic coast
AV Baranskaya, NS Khan, FA Romanenko… - Quaternary Science …, 2018 - Elsevier
We present the first quality-controlled relative sea-level (RSL) database for the Russian
Arctic coast from the Barents Sea in the west to Laptev Sea in the east (29–152 o E and 63 …
Arctic coast from the Barents Sea in the west to Laptev Sea in the east (29–152 o E and 63 …
Numerical simulations of the Cordilleran ice sheet through the last glacial cycle
After more than a century of geological research, the Cordilleran ice sheet of North America
remains among the least understood in terms of its former extent, volume, and dynamics …
remains among the least understood in terms of its former extent, volume, and dynamics …
The Bothnian Sea ice stream: early Holocene retreat dynamics of the south‐central Fennoscandian Ice Sheet
The Gulf of Bothnia hosted a variety of palaeo‐glaciodynamic environments throughout the
growth and decay of the last Fennoscandian Ice Sheet, from the main ice‐sheet divide to a …
growth and decay of the last Fennoscandian Ice Sheet, from the main ice‐sheet divide to a …
Subglacial water storage and drainage beneath the Fennoscandian and Barents Sea ice sheets
Subglacial hydrology modulates how ice sheets flow, respond to climate, and deliver
meltwater, sediment and nutrients to proglacial and marine environments. Here, we …
meltwater, sediment and nutrients to proglacial and marine environments. Here, we …
[HTML][HTML] Left high and dry: deglaciation of Dogger Bank, North Sea, recorded in proglacial lake evolution
Reconstructions of palaeo-ice sheet retreat in response to climate warming using offshore
archives can provide vital analogues for future ice-sheet behaviour. At the Last Glacial …
archives can provide vital analogues for future ice-sheet behaviour. At the Last Glacial …