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-glacial cycles. Our efficient solution includes both a fast yet accurate deep learning-based estimation of high- order ice flows and a new, multi-scale advection scheme enabling us to account for the distinct time scales at which glaciers reach equilibrium compared to eroding the terrain. We combine the resulting glacial erosion model with finer-scale erosive phenomena to account for the transport of debris flowing from cliffs. This enables us to model the formation of terrain shapes not previously adequately modeled in Computer Graphics, ranging from...
At middle to high latitudes, many alpine valleys have been shaped by glaciers associated with period...
Glaciers are highly effective agents of erosion that have profoundly shaped Earth's surface, but the...
Le Cénozoïque est marqué par un refroidissement global du climat et des périodes glaciaires/intergla...
International audienceWe introduce the first solution for simulating the formation and evolution of ...
This thesis details the application of numerical modelling techniques to simulate erosion under ice...
Pietro Sternai : Now at: the Institut desSciences de laTerre d'Orléans - (ISTO), University of Orléa...
International audienceA new version of a landscape evolution model that includes the evolution of an...
One of the most fundamental insights for understanding how landscapes evolve is based on determining...
Modeling glacial landform evolution is more challenging than modeling fluvial landform evolution. Wh...
Mountain topography is constructed through a variety of interacting processes. Over glaciological ti...
Ice can sculpt extraordinary landscapes, yet the efficacy of, and controls governing, glacial erosio...
The Cenozoic is marked by a global climatic cooling and glacial/interglacial periods which intensifi...
Glacial inversion modelling of continental-scale palaeo-ice sheets is now recognized as an important...
In order to extend our knowledge of glacial relief production in mountainous areas new methods are r...
Quarrying of bedrock is a primary agent of subglacial erosion. Although the mechanical theory behind...
At middle to high latitudes, many alpine valleys have been shaped by glaciers associated with period...
Glaciers are highly effective agents of erosion that have profoundly shaped Earth's surface, but the...
Le Cénozoïque est marqué par un refroidissement global du climat et des périodes glaciaires/intergla...
International audienceWe introduce the first solution for simulating the formation and evolution of ...
This thesis details the application of numerical modelling techniques to simulate erosion under ice...
Pietro Sternai : Now at: the Institut desSciences de laTerre d'Orléans - (ISTO), University of Orléa...
International audienceA new version of a landscape evolution model that includes the evolution of an...
One of the most fundamental insights for understanding how landscapes evolve is based on determining...
Modeling glacial landform evolution is more challenging than modeling fluvial landform evolution. Wh...
Mountain topography is constructed through a variety of interacting processes. Over glaciological ti...
Ice can sculpt extraordinary landscapes, yet the efficacy of, and controls governing, glacial erosio...
The Cenozoic is marked by a global climatic cooling and glacial/interglacial periods which intensifi...
Glacial inversion modelling of continental-scale palaeo-ice sheets is now recognized as an important...
In order to extend our knowledge of glacial relief production in mountainous areas new methods are r...
Quarrying of bedrock is a primary agent of subglacial erosion. Although the mechanical theory behind...
At middle to high latitudes, many alpine valleys have been shaped by glaciers associated with period...
Glaciers are highly effective agents of erosion that have profoundly shaped Earth's surface, but the...
Le Cénozoïque est marqué par un refroidissement global du climat et des périodes glaciaires/intergla...