[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 …
Glacial geomorphological map**: A review of approaches and frameworks for best practice
Geomorphological map** 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 …
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 …
Precise date for the Laacher See eruption synchronizes the Younger Dryas
Abstract The Laacher See eruption (LSE) in Germany ranks among Europe's largest
volcanic events of the Upper Pleistocene,. Although tephra deposits of the LSE represent an …
volcanic events of the Upper Pleistocene,. Although tephra deposits of the LSE represent an …
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 isostatic adjustment modelling: historical perspectives, recent advances, and future directions
PL Whitehouse - Earth surface dynamics, 2018 - esurf.copernicus.org
Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …
Complex spatio-temporal structure of the Holocene Thermal Maximum
Inconsistencies between Holocene climate reconstructions and numerical model
simulations question the robustness of climate models and proxy temperature records …
simulations question the robustness of climate models and proxy temperature records …
A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting
The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
[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 extreme yet transient nature of glacial erosion
Ice can sculpt extraordinary landscapes, yet the efficacy of, and controls governing, glacial
erosion on geological timescales remain poorly understood and contended, particularly …
erosion on geological timescales remain poorly understood and contended, particularly …