[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 …
Pattern and timing of retreat of the last British-Irish Ice Sheet
During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …
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 …
[書籍][B] Reconstructing quaternary environments
This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …
and updated to provide a new account of the history and scale of environmental changes …
Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction
The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
[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 …
A stratigraphical basis for the Last Glacial Maximum (LGM)
Abstract The Last Glacial Maximum (LGM) is widely used to refer to the episode when global
ice volume last reached its maximum and associated sea levels were at their lowest …
ice volume last reached its maximum and associated sea levels were at their lowest …
An improved glacial isostatic adjustment model for the British Isles
The glacial isostatic adjustment (GIA) of the British Isles is of interest due to the constraints
that can be provided on key model parameters such as the global meltwater signal, local ice …
that can be provided on key model parameters such as the global meltwater signal, local ice …
On the reconstruction of palaeo-ice sheets: recent advances and future challenges
Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …
mechanisms of global climate change and associated sea-level fluctuations in the past …
Millennial-scale fluctuations of the European Ice Sheet at the end of the last glacial, and their potential impact on global climate
Abstract Reconstructing Northern Hemisphere ice-sheet oscillations and meltwater routing
to the ocean is important to better understand the mechanisms behind abrupt climate …
to the ocean is important to better understand the mechanisms behind abrupt climate …