Zobrazeno 1 - 10
of 147
pro vyhledávání: '"O. Marc"'
Publikováno v:
Earth Surface Dynamics, Vol 12, Pp 863-881 (2024)
Landslides influence fluvial suspended sediment transport by changing sediment supply and grain size, which alter suspended sediment concentrations and fluxes for a period of time after landsliding. To investigate the duration and scale of altered su
Externí odkaz:
https://doaj.org/article/5b1f5f3693304e67a713521232dc069a
Publikováno v:
Earth Surface Dynamics, Vol 11, Pp 1117-1143 (2023)
Debris flows regularly traverse bedrock channels that dissect steep landscapes, but our understanding of bedrock erosion by debris flows and their impact on steepland morphology is still rudimentary. Quantitative models of steep bedrock channel netwo
Externí odkaz:
https://doaj.org/article/f5202a1e362f463cac07625e1507658b
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023)
Abstract Monsoon rainfall triggers hundreds of landslides across Nepal every year, causing significant hazard and mass wasting. Annual inventories of these landslides have been mapped using multi‐spectral satellite images, but these images are obsc
Externí odkaz:
https://doaj.org/article/2ae41e0201e042439b580d2417070d39
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 22, Pp 2637-2653 (2022)
Heavy-rainfall events in mountainous areas trigger destructive landslides, which pose a risk to people and infrastructure and significantly affect the landscape. Landslide locations are commonly mapped using optical satellite imagery, but in some reg
Externí odkaz:
https://doaj.org/article/3d53042b79c74bbdaef82be4179ea13c
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 22, Pp 1129-1149 (2022)
Landslides are a key hazard in high-relief areas around the world and pose a risk to populations and infrastructure. It is important to understand where landslides are likely to occur in the landscape to inform local analyses of exposure and potentia
Externí odkaz:
https://doaj.org/article/7bd66698e5fe43b28afd13e842c805bf
Publikováno v:
Earth Surface Dynamics, Vol 9, Pp 995-1011 (2021)
The size of grains delivered to rivers by hillslope processes is thought to be a key factor controlling sediment transport, long-term erosion and the information recorded in sedimentary archives. Recently, models have been developed to estimate the g
Externí odkaz:
https://doaj.org/article/6360ee210b4d4539b345ea12384a34eb
Publikováno v:
Earth Surface Dynamics, Vol 7, Pp 829-839 (2019)
The large, shallow earthquakes at Northridge, California (1994), Chi-Chi, Taiwan (1999), and Wenchuan, China (2008), each triggered thousands of landslides. We have determined the position of these landslides along hillslopes, normalizing for statist
Externí odkaz:
https://doaj.org/article/a1c9b15d29c64601908f0d9947307d95
Publikováno v:
Earth Surface Dynamics, Vol 7, Pp 107-128 (2019)
In active mountain belts with steep terrain, bedrock landsliding is a major erosional agent. In the Himalayas, landsliding is driven by annual hydro-meteorological forcing due to the summer monsoon and by rarer, exceptional events, such as earthquake
Externí odkaz:
https://doaj.org/article/5411f2a7aa51499eb203377601e72701
Publikováno v:
Earth Surface Dynamics, Vol 6, Pp 903-922 (2018)
Rainfall-induced landslides are a common and significant source of damages and fatalities worldwide. Still, we have little understanding of the quantity and properties of landsliding that can be expected for a given storm and a given landscape, mo
Externí odkaz:
https://doaj.org/article/dc348344b775430782f5497543676094
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 17, Pp 1159-1175 (2017)
We present an analytical, seismologically consistent expression for the surface area of the region within which most landslides triggered by an earthquake are located (landslide distribution area). This expression is based on scaling laws relating
Externí odkaz:
https://doaj.org/article/454456853c3a4526b6a27fb6cb80046c