An updated radiocarbon-based ice margin chronology for the last deglaciation of the North American Ice Sheet Complex
Abstract The North American Ice Sheet Complex (NAISC; consisting of the Laurentide,
Cordilleran and Innuitian ice sheets) was the largest ice mass to repeatedly grow and decay …
Cordilleran and Innuitian ice sheets) was the largest ice mass to repeatedly grow and decay …
[HTML][HTML] The evolution of the Patagonian Ice Sheet from 35 ka to the present day (PATICE)
We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …
Changing state of the climate system
2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
The configuration of Northern Hemisphere ice sheets through the Quaternary
Our understanding of how global climatic changes are translated into ice-sheet fluctuations
and sea-level change is currently limited by a lack of knowledge of the configuration of ice …
and sea-level change is currently limited by a lack of knowledge of the configuration of ice …
[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 …
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 …
Glacial geomorphological mapping: A review of approaches and frameworks for best practice
Geomorphological mapping is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …
processes and landscape evolution in a range of environmental contexts. In glacial …
[HTML][HTML] Reconciling records of ice streaming and ice margin retreat to produce a palaeogeographic reconstruction of the deglaciation of the Laurentide Ice Sheet
This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …
The international bathymetric chart of the Arctic Ocean version 4.0
M Jakobsson, LA Mayer, C Bringensparr, CF Castro… - Scientific data, 2020 - nature.com
Bathymetry (seafloor depth), is a critical parameter providing the geospatial context for a
multitude of marine scientific studies. Since 1997, the International Bathymetric Chart of the …
multitude of marine scientific studies. Since 1997, the International Bathymetric Chart of the …
The Bering Strait was flooded 10,000 years before the last glacial maximum
The cyclic growth and decay of continental ice sheets can be reconstructed from the history
of global sea level. Sea level is relatively well constrained for the Last Glacial Maximum …
of global sea level. Sea level is relatively well constrained for the Last Glacial Maximum …