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Quantifying rates of landscape evolution and tectonic processes by thermochronology and numerical modeling of crustal heat transport using PECUBE
PECUBE is a three-dimensional thermal–kinematic code capable of solving the heat
production–diffusion–advection equation under a temporally varying surface boundary …
production–diffusion–advection equation under a temporally varying surface boundary …
Ice‐Dynamical Glacier Evolution Modeling—A Review
Glaciers play a crucial role in the Earth System: they are important water suppliers to lower‐
lying areas during hot and dry periods, and they are major contributors to the observed …
lying areas during hot and dry periods, and they are major contributors to the observed …
Modelling the feedbacks between mass balance, ice flow and debris transport to predict the response to climate change of debris-covered glaciers in the Himalaya
Many Himalayan glaciers are characterised in their lower reaches by a rock debris layer.
This debris insulates the glacier surface from atmospheric warming and complicates the …
This debris insulates the glacier surface from atmospheric warming and complicates the …
Forming terrains by glacial erosion
We introduce the first solution for simulating the formation and evolution of glaciers, together
with their attendant erosive effects, for periods covering the combination of glacial and inter …
with their attendant erosive effects, for periods covering the combination of glacial and inter …
Glacial hydrology and erosion patterns: a mechanism for carving glacial valleys
Most glacial erosion models assume that erosion rates are proportional to ice-sliding
velocity. While recent studies have shown that water plays a major role in modulating sliding …
velocity. While recent studies have shown that water plays a major role in modulating sliding …
Reconstructing climate from glaciers
AN Mackintosh, BM Anderson… - Annual Review of …, 2017 - annualreviews.org
Glaciers offer the potential to reconstruct past climate over timescales from decades to
millennia. They are found on nearly every continent, and at the Last Glacial Maximum …
millennia. They are found on nearly every continent, and at the Last Glacial Maximum …
A simple inverse method for the distribution of basal sliding coefficients under ice sheets, applied to Antarctica
D Pollard, RM DeConto - The Cryosphere, 2012 - tc.copernicus.org
Variations in intrinsic bed conditions that affect basal sliding, such as the distribution of
deformable sediment versus hard bedrock, are important boundary conditions for large …
deformable sediment versus hard bedrock, are important boundary conditions for large …
Forecasting the response of Earth's surface to future climatic and land use changes: A review of methods and research needs
In the future, Earth will be warmer, precipitation events will be more extreme, global mean
sea level will rise, and many arid and semiarid regions will be drier. Human modifications of …
sea level will rise, and many arid and semiarid regions will be drier. Human modifications of …
Glaciations in response to climate variations preconditioned by evolving topography
Landscapes modified by glacial erosion show a distinct distribution of surface area with
elevation,,(hypsometry). In particular, the height of these regions is influenced by climatic …
elevation,,(hypsometry). In particular, the height of these regions is influenced by climatic …
Formation of plateau landscapes on glaciated continental margins
Low-relief plateaus separated by deeply incised fjords are hallmarks of glaciated, passive
continental margins. Spectacular examples fringe the once ice-covered North Atlantic coasts …
continental margins. Spectacular examples fringe the once ice-covered North Atlantic coasts …