Articles | Volume 13, issue 9
https://doi.org/10.5194/gmd-13-3863-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-13-3863-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
HyLands 1.0: a hybrid landscape evolution model to simulate the impact of landslides and landslide-derived sediment on landscape evolution
Benjamin Campforts
CORRESPONDING AUTHOR
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, USA
Charles M. Shobe
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
Philippe Steer
Géosciences Rennes – UMR 6118, CNRS, Université de Rennes, Rennes, France
Matthias Vanmaercke
Département de Géographie, UR SPHERES, Université de Liège, Liège, Belgium
Dimitri Lague
Géosciences Rennes – UMR 6118, CNRS, Université de Rennes, Rennes, France
Jean Braun
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
Institute of Earth and Environmental Science, Universität Potsdam, Potsdam, Germany
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Cited
28 citations as recorded by crossref.
- The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards C. Shobe et al. 10.1016/j.earscirev.2021.103717
- Controls on the grain size distribution of landslides in Taiwan: the influence of drop height, scar depth and bedrock strength O. Marc et al. 10.5194/esurf-9-995-2021
- Uncertainties in landslide susceptibility prediction modeling: A review on the incompleteness of landslide inventory and its influence rules F. Huang et al. 10.1016/j.gsf.2024.101886
- The scaling of landslide-dammed lakes A. Argentin et al. 10.1016/j.gloplacha.2023.104190
- The concept of event-size-dependent exhaustion and its application to paraglacial rockslides S. Hergarten 10.5194/nhess-23-3051-2023
- Rethinking Variability in Bedrock Rivers: Sensitivity of Hillslope Sediment Supply to Precipitation Events Modulates Bedrock Incision During Floods C. DeLisle & B. Yanites 10.1029/2023JF007148
- CHONK 1.0: landscape evolution framework: cellular automata meets graph theory B. Gailleton et al. 10.5194/gmd-17-71-2024
- The Fate of Sediment After a Large Earthquake O. Francis et al. 10.1029/2021JF006352
- Identification of Streamside Landslides with the Use of Unmanned Aerial Vehicles (UAVs) in Greece, Romania, and Turkey M. Yavuz et al. 10.3390/rs15041006
- The Art of Landslides: How Stochastic Mass Wasting Shapes Topography and Influences Landscape Dynamics B. Campforts et al. 10.1029/2022JF006745
- Earthquake-induced landslides coupled to fluvial incision in Andean Patagonia: Inferring their effects on landscape at geological time scales B. Morales et al. 10.1016/j.geomorph.2023.108731
- Frost cracking dictated landslide distribution in response to temperature change since Last Glacial Maximum across the Eastern Qilian Mountains H. Geng et al. 10.1002/esp.5450
- Impacts of Spontaneous Waterfall Development on Bedrock River Longitudinal Profile Morphology S. Rothman et al. 10.1029/2022JF007057
- Anthropogenic impacts on Holocene fluvial dynamics in the Chinese Loess Plateau, an evaluation based on landscape evolution modeling H. Chen et al. 10.1016/j.geomorph.2021.107935
- Do standing trees affect landslide mobility on forested hillslopes in Japan? H. Tsunetaka et al. 10.1002/esp.5461
- Evidence of Seattle Fault Earthquakes from Patterns in Deep-Seated Landslides E. Herzig et al. 10.1785/0120230079
- Impacts of Rainstorm Intensity and Temporal Pattern on Caprock Cliff Persistence and Hillslope Morphology in Drylands Y. Shmilovitz et al. 10.1029/2023JF007478
- Remote Sensing of Landslide-Generated Sediment Plumes, Peace River, British Columbia K. Hughes et al. 10.3390/rs13234901
- Past anthropogenic land use change caused a regime shift of the fluvial response to Holocene climate change in the Chinese Loess Plateau H. Chen et al. 10.5194/esurf-12-163-2024
- Geomorphometric assessment of spatial transfer potential of landslides sediment in seismically impacted areas J. Xiong et al. 10.1007/s11069-024-07034-w
- CSDMS: a community platform for numerical modeling of Earth surface processes G. Tucker et al. 10.5194/gmd-15-1413-2022
- CRHyME (Climatic Rainfall Hydrogeological Modelling Experiment): a new model for geo-hydrological hazard assessment at the basin scale A. Abbate et al. 10.5194/nhess-24-501-2024
- Evaluation of machine learning-based algorithms for landslide detection across satellite sensors for the 2019 Cyclone Idai event, Chimanimani District, Zimbabwe R. Das & K. Wegmann 10.1007/s10346-022-01912-9
- Two multi-temporal datasets to track debris flow after the 2008 Wenchuan earthquake L. Wang et al. 10.1038/s41597-022-01658-y
- Modelling detrital cosmogenic nuclide concentrations during landscape evolution in Cidre v2.0 S. Carretier et al. 10.5194/gmd-16-6741-2023
- How landslide sediments are transferred out of an alpine basin: Evidence from the epicentre of the Wenchuan earthquake J. Xiong et al. 10.1016/j.catena.2021.105781
- A landslide runout model for sediment transport, landscape evolution, and hazard assessment applications J. Keck et al. 10.5194/esurf-12-1165-2024
- The influence of landslide morphology on erosion rate variability across western Himalayan catchments: Role of westerlies and summer monsoon interaction in the landscape characterization A. Kashyap & M. Behera 10.1002/gj.4913
27 citations as recorded by crossref.
- The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards C. Shobe et al. 10.1016/j.earscirev.2021.103717
- Controls on the grain size distribution of landslides in Taiwan: the influence of drop height, scar depth and bedrock strength O. Marc et al. 10.5194/esurf-9-995-2021
- Uncertainties in landslide susceptibility prediction modeling: A review on the incompleteness of landslide inventory and its influence rules F. Huang et al. 10.1016/j.gsf.2024.101886
- The scaling of landslide-dammed lakes A. Argentin et al. 10.1016/j.gloplacha.2023.104190
- The concept of event-size-dependent exhaustion and its application to paraglacial rockslides S. Hergarten 10.5194/nhess-23-3051-2023
- Rethinking Variability in Bedrock Rivers: Sensitivity of Hillslope Sediment Supply to Precipitation Events Modulates Bedrock Incision During Floods C. DeLisle & B. Yanites 10.1029/2023JF007148
- CHONK 1.0: landscape evolution framework: cellular automata meets graph theory B. Gailleton et al. 10.5194/gmd-17-71-2024
- The Fate of Sediment After a Large Earthquake O. Francis et al. 10.1029/2021JF006352
- Identification of Streamside Landslides with the Use of Unmanned Aerial Vehicles (UAVs) in Greece, Romania, and Turkey M. Yavuz et al. 10.3390/rs15041006
- The Art of Landslides: How Stochastic Mass Wasting Shapes Topography and Influences Landscape Dynamics B. Campforts et al. 10.1029/2022JF006745
- Earthquake-induced landslides coupled to fluvial incision in Andean Patagonia: Inferring their effects on landscape at geological time scales B. Morales et al. 10.1016/j.geomorph.2023.108731
- Frost cracking dictated landslide distribution in response to temperature change since Last Glacial Maximum across the Eastern Qilian Mountains H. Geng et al. 10.1002/esp.5450
- Impacts of Spontaneous Waterfall Development on Bedrock River Longitudinal Profile Morphology S. Rothman et al. 10.1029/2022JF007057
- Anthropogenic impacts on Holocene fluvial dynamics in the Chinese Loess Plateau, an evaluation based on landscape evolution modeling H. Chen et al. 10.1016/j.geomorph.2021.107935
- Do standing trees affect landslide mobility on forested hillslopes in Japan? H. Tsunetaka et al. 10.1002/esp.5461
- Evidence of Seattle Fault Earthquakes from Patterns in Deep-Seated Landslides E. Herzig et al. 10.1785/0120230079
- Impacts of Rainstorm Intensity and Temporal Pattern on Caprock Cliff Persistence and Hillslope Morphology in Drylands Y. Shmilovitz et al. 10.1029/2023JF007478
- Remote Sensing of Landslide-Generated Sediment Plumes, Peace River, British Columbia K. Hughes et al. 10.3390/rs13234901
- Past anthropogenic land use change caused a regime shift of the fluvial response to Holocene climate change in the Chinese Loess Plateau H. Chen et al. 10.5194/esurf-12-163-2024
- Geomorphometric assessment of spatial transfer potential of landslides sediment in seismically impacted areas J. Xiong et al. 10.1007/s11069-024-07034-w
- CSDMS: a community platform for numerical modeling of Earth surface processes G. Tucker et al. 10.5194/gmd-15-1413-2022
- CRHyME (Climatic Rainfall Hydrogeological Modelling Experiment): a new model for geo-hydrological hazard assessment at the basin scale A. Abbate et al. 10.5194/nhess-24-501-2024
- Evaluation of machine learning-based algorithms for landslide detection across satellite sensors for the 2019 Cyclone Idai event, Chimanimani District, Zimbabwe R. Das & K. Wegmann 10.1007/s10346-022-01912-9
- Two multi-temporal datasets to track debris flow after the 2008 Wenchuan earthquake L. Wang et al. 10.1038/s41597-022-01658-y
- Modelling detrital cosmogenic nuclide concentrations during landscape evolution in Cidre v2.0 S. Carretier et al. 10.5194/gmd-16-6741-2023
- How landslide sediments are transferred out of an alpine basin: Evidence from the epicentre of the Wenchuan earthquake J. Xiong et al. 10.1016/j.catena.2021.105781
- A landslide runout model for sediment transport, landscape evolution, and hazard assessment applications J. Keck et al. 10.5194/esurf-12-1165-2024
Latest update: 13 Dec 2024
Short summary
Landslides shape the Earth’s surface and are a dominant source of terrestrial sediment. Rivers, then, act as conveyor belts evacuating landslide-produced sediment. Understanding the interaction among rivers and landslides is important to predict the Earth’s surface response to past and future environmental changes and for mitigating natural hazards. We develop HyLands, a new numerical model that provides a toolbox to explore how landslides and rivers interact over several timescales.
Landslides shape the Earth’s surface and are a dominant source of terrestrial sediment....